Entries |
Document | Title | Date |
20080215246 | MEASURING AND MODIFYING DIRECTIONALITY OF SEISMIC INTERFEROMETRY DATA - Methods and apparatuses are disclosed for replacing the individual receivers used with a seismic interferometry process with an array of seismic receivers and then manipulating the array data in order to measure and modify the typical non-uniform directionality function of the background seismic energy. The non-uniform directionality function is a significant cause of noise with seismic interferometry. Furthermore, the array of receivers may be used to significantly enhance the preferred reflection energy and damp undesirable near surface energy. The directionality function may be modified by using an array of receivers for the virtual source location of seismic interferometry to measure the non-uniform directionality function, generating multiplication factors, and applying the multiplication factors to convert the measured directionality function into a desired directionality function. | 09-04-2008 |
20080228402 | Processing of Seismic Data Acquired Using Twin Over/Under Streamers - A method for processing seismic data acquired using a first over/under streamer and a second over/under streamer. In one implementation, the method may include estimating seismic data that would have been acquired by a third over/under streamer disposed at a depth equivalent to a distance separating the first over/under streamer from the second over/under streamer; and applying a dephase and sum algorithm to seismic data acquired by the first over/under streamer and the second over/under streamer and the estimated seismic data. | 09-18-2008 |
20080228403 | Technique to Provide Seismic Data-Based Products - A technique includes providing a pricing scheme to sell at least one seismic data-based product. The seismic data-based product(s) are generated from seismic data that is obtained from at least one sensor in tow, and the seismic data includes particle motion data, which the pricing scheme excludes from being sold. | 09-18-2008 |
20080275649 | Method for Optimal Wave Field Separation - A technique for decomposing a recorded wave field represented in a set of multicomponent, marine seismic data centers around a computer-implemented method including: estimating the statistics of the noise terms in each one of a predetermined group of seismic measurements in a seismic data set acquired in a marine survey; modeling the physical propagation of a recorded wave field represented in the seismic data set from the estimated statistics; and estimating a directional component of the recorded wave field from the physical propagation model that minimizes error relative to the seismic measurements. | 11-06-2008 |
20080275650 | METHOD OF AND APPARATUS FOR PROCESSING SEISMIC DATA - A method of processing seismic data that includes including first and second modes of seismic energy where the second mode has been generated by partial mode conversion of the first mode at a boundary face of a layer of the seabed includes the step of cross-correlating a trace acquired at a receiver and including events corresponding to the first mode with a trace acquired at the same receiver and including events corresponding to the second mode. An event in the cross-correlated data that corresponds to partial mode conversion is identified, and the amplitude of this event is normalized, for example relative to the amplitude of the peak in the cross-correlogram at zero time delay. Information about the effects of the static shift produced by the layer and/or about vector infidelity can be arrived from normalized cross-correlograms for receivers in a receiver array. | 11-06-2008 |
20080294345 | METHOD FOR DETERMINING ATTRIBUTES ASSOCIATED WITH NET-SAND THICKNESS - The present invention provides a method for determining net-sand thickness and net-reservoir volume over a broad range of gross sand thickness in a target zone. A net-resource attribute is designed to estimate net-sand thickness based upon the inner product of the determined probe function and the segment of the seismic trace that includes the target zone. The net-resource attribute and the geographic location for each trace can be stored and a net-resource table may be created. Maps and net-reservoir volume can be generated from the geographical location information and the net-resource attributes. Net-sand thickness allows the determination of the total volume of sand and thus the size of the hydrocarbon container or the net-reservoir volume. | 11-27-2008 |
20090012712 | Assisted Seismic Measuring System Including GPS Receivers - A system for analyzing three-dimensional seismic data includes a plurality of digitizer units, each with a configuration of geophones, a data recording and control center, a base GPS receiver with an associated antenna with a substantially unrestricted view of the sky and at the respective digitizer units low-power slave GPS receivers that acquire and track GPS satellite signals using tracking assistance information provided by the base GPS receiver. The slave GPS receivers use the tracking assistance information to acquire and track GPS satellite signals that may be relatively weak at the receivers, due to conditions at the site, such as foliage canopies and so forth. The system processes range information provided by the slave GPS receivers over an extended period of time. In this way, the precise positions of the respective slave GPS receivers, and thus, the digitizer units, can be calculated, even if the slave GPS receivers are able to observe and collect data from sets of two or more satellites for only three or four relatively short time intervals at various sky positions during the extended period. The slave GPS receivers then locally produce for the digitizer units timing signals that are based on the GPS codes and synchronized across the system. If a given slave GPS receiver cannot, at a given time, track any GPS satellite signals, a nearby slave GPS receiver supplies the timing information required for the geophone data gathering operations. | 01-08-2009 |
20090024328 | PROCESSING SEISMIC DATA USING INTERFEROMETRY TECHNIQUES - Method for processing seismic data. In one implementation, the method includes converting a common midpoint (CMP) gather of seismograms into one or more interferogram common midpoint (ICMP) gathers, generating a semblance spectrum for each ICMP gather, stacking the semblance spectrum from each ICMP gather to generate a combined semblance spectrum and deriving a normal moveout (NMO) velocity profile from the combined semblance spectrum. | 01-22-2009 |
20090037114 | 4D+ PRESTACK SEISMIC DATA STRUCTURE, AND METHODS AND APPARATUS FOR PROCESSING 4D+ PRESTACK SEISMIC DATA - Methods, apparatus and products for processing 4D+ prestack seismic data having the form of 3D prestack gathers, single fold 3D volumes, and a mapping table to link the gathers and the volumes coherently. | 02-05-2009 |
20090037115 | METHOD FOR DETERMINING SEISMIC DATA QUALITY - The present invention determines seismic data quality for a plurality of locations within a seismic survey for a geologic or geophysical region of interest. The present invention additionally includes generating correlation coefficients which relate to the seismic data quality so that the seismic data quality can be incorporated into geostatistical analyses associated with decisions that are based in part on the seismic survey. | 02-05-2009 |
20090043511 | Assisted Seismic Measuring System Including GPS Receivers - A system for analyzing three-dimensional seismic data includes a plurality of digitizer units, each with a configuration of geophones, a data recording and control center, a base GPS receiver with an associated antenna with a substantially unrestricted view of the sky and at the respective digitizer units low-power slave GPS receivers that acquire and track GPS satellite signals using tracking assistance information provided by the base GPS receiver. The slave GPS receivers use the tracking assistance information to acquire and track GPS satellite signals that may be relatively weak at the receivers, due to conditions at the site, such as foliage canopies and so forth. The system processes range information provided by the slave GPS receivers over an extended period of time. In this way, the precise positions of the respective slave GPS receivers, and thus, the digitizer units, can be calculated, even if the slave GPS receivers are able to observe and collect data from sets of two or more satellites for only three or four relatively short time intervals at various sky positions during the extended period. The slave GPS receivers then locally produce for the digitizer units timing signals that are based on the GPS codes and synchronized across the system. If a given slave GPS receiver cannot, at a given time, track any GPS satellite signals, a nearby slave GPS receiver supplies the timing information required for the geophone data gathering operations. | 02-12-2009 |
20090048784 | 3D SURFACE RELATED MULTIPLE ELIMINATION FOR WIDE AZIMUTH SEISMIC DATA - According to a preferred aspect of the instant invention, there is provided herein a system and method for the imaging and monitoring of the subsurface hydrocarbon reservoirs and other subsurface features, wherein the collected seismic data contain multiples therein. In brief, the instant invention is a method of removing multiples using SRME, wherein wide azimuth seismic data are used to directly compute a multiple prediction via a mixed space-wavenumber-frequency domain implementation. | 02-19-2009 |
20090093963 | METHOD FOR QUANTITATIVE EVALUATION OF FLUID PRESSURES AND DETECTION OF OVERPRESSURES IN AN UNDERGROUND MEDIUM - Method for evaluating fluid pressures in an underground zone by means of seismic and well data. The zone studied is divided into several time analysis intervals. For each of these intervals, a pre-stack stratigraphic inversion of the seismic data is then carried out using geological a priori information, and a lithoseismic facies cube is determined by lithoseismic analysis. Then, for each facies, relations connecting the seismic impedances of wells to differential pressures in wells are determined in each analysis interval. Finally, a differential pressure cube is determined using the previous relations, as well as a confining pressure cube, in order to determine the fluid pressures in the subsoil by simple difference between these two cubes. Application: petroleum sphere for the detection of overpressure zones during drilling for example. | 04-09-2009 |
20090093964 | MULTI-DIMENSIONAL PARAMETER IDENTIFICATION METHOD AND DEVICE: APPLICATION TO THE LOCATION AND RECONSTRUCTION OF DEEP ELECTRICAL ACTIVITIES BY MEANS OF SURFACE OBSERVATIONS - A method is provided for identifying multidimensional parameters of a plurality of P>1 sources of interest present in a predetermined multidimensional conductive environment by a plurality of observations ( | 04-09-2009 |
20090093965 | DETERMINING FAULT TRANSMISSIVITY IN A SUBTERRANEAN RESERVOIR - To determine fault transmissivity in a subterranean reservoir, fault structures in the subterranean reservoir are identified, and elastic impedance data is computed from well log data and seismic data. Normalization parameters that have a predetermined orientation with respect to the identified fault structures are computed, and elastic impedance flux values are normalized with respect to the normalization parameters, where the normalized elastic impedance flux values are indicative of transmissivities of fault structures in the subterranean structure. | 04-09-2009 |
20090099778 | SEISMIC DATA PROCESSING WORKFLOW DECISION TREE - Implementations of various technologies for a method for modifying a seismic data processing workflow. In one implementation, the method may include displaying the seismic data processing workflow in a hierarchical structure. The hierarchical structure may have one or more branches and one or more nodes. Each branch may represent a parameter value. Each node may represent a data output of a seismic data process performed with the parameter value. A selection of a node may be received. A graphical representation of the data output for the selected node may be displayed. | 04-16-2009 |
20090112477 | Correction for Errors Caused by Variation in Water Conditions - Method for processing seismic data to correct for errors caused by variation in water conditions. In one implementation, the method may include (a) applying a dip correction to a plurality of observed water bottom reflection times using a model water velocity and an estimate of geologic dip; (b) applying a normal moveout (NMO) correction to the dip corrected observed water bottom reflection times using the model water velocity; (c) applying a common mid point (“CMP”) bin centering correction to the NMO corrected, dip corrected observed water bottom reflection times using the model water velocity and the estimate of geologic dip; (d) solving for Δs | 04-30-2009 |
20090192718 | SUBSURFACE PREDICTION METHOD AND SYSTEM - A method of predicting subsurface properties of a geologic formation includes acquiring seismic data for a subsurface region including the geologic formation of interest, computing seismic attributes of the measured seismic data over at least part of this geologic formation, determining internally consistent rock properties representative of the geologic formation, generating models of the same part of the geologic formation with these rock properties, computing synthetic seismic data from the models, computing the same attributes from these synthetic seismic data, and using Bayesian analysis to predict, from the probability of modeled attributes given the models, the probability of the actual subsurface properties given the measured attributes. | 07-30-2009 |
20090204330 | SYSTEM AND METHOD FOR USING TIME-DISTANCE CHARACTERISTICS IN ACQUISITION, PROCESSING, AND IMAGING OF T-CSEM DATA - There is provided herein a system and method of acquiring, processing, and imaging transient Controlled Source ElectroMagnetic (t-CSEM) data in ways that are similar to those used for seismic data. In particular, the instant invention exploits the time-distance characteristics of t-CSEM data to permit the design and execution of t-CSEM surveys for optimal subsequent processing and imaging. The instant invention illustrates how to correct t-CSEM data traces for attenuation and dispersion, so that their characteristics are more like those of seismic data and can be processed using algorithms familiar to the seismic processor. The resulting t-CSEM images, particularly if combined with corresponding seismic images, may be used to infer the location of hydrocarbon reservoirs. | 08-13-2009 |
20090222210 | Method for determining the earthquake protection of buildings - According to the invention, in the method for determining the earthquake protection of buildings, the natural frequency of a building is determined. Moreover, the natural frequency of the ground surrounding the building is determined. Thereafter, a rating value for the building is calculated based on a comparison of the natural frequency of the building to the natural frequency of the ground. Based on this rated value, the earthquake protection of a building can be determined. Preferably, a failure probability for the building and an average damage to the building are calculated on the basis of the rating value, depending on the magnitude of the earthquake. | 09-03-2009 |
20090240438 | System and method for migrating seismic data - A system and method that enable the processing of seismic data. In one embodiment, a system comprises a plurality of processing nodes and a server. The plurality of processing nodes are configured to process seismic data for migration. The server is operatively linked to each of the plurality of processing nodes to enable communication between the server and the processing nodes. The server may manage a set of stored beam tables that can be accessed by the processing nodes in order to process seismic data. | 09-24-2009 |
20090259405 | METHODS, SYSTEMS, AND COMPUTER-READABLE MEDIA FOR GENERATING SEISMIC EVENT TIME HISTORIES - Methods, systems, and computer-readable media generate acceleration time histories. An initial acceleration history is applied to a response model with natural frequencies across a spectrum of interest to develop a displacement response. Low-frequency enhancement signals are determined by comparing the displacement response to a standard displacement response. The enhancement signals are combined with the initial acceleration history to develop a second acceleration history, which is applied to the response model to develop an acceleration response. High-frequency enhancement signals are determined by comparing the acceleration response to a standard acceleration response. The enhancement signals are combined with the second acceleration history to develop a desired acceleration history. Acceleration histories also may be created by adding random phase angles at various frequencies to an initial acceleration history in the frequency domain, which is then converted to the time domain and scaled to generate a low-correlation history. | 10-15-2009 |
20090259406 | CONTINUOUS MICROSEISMIC MAPPING FOR REAL-TIME 3D EVENT DETECTION AND LOCATION - A method for the detection and localization of microseismic events is proposed which operates in real-time. It provides hypocenters in three spatial dimensions along with an estimate of the event origin time. Sensor positions may be distributed in 3D space, and are not confined to linear arrays in vertical wells. The method combines and improves two existing approaches. For detection and localization purposes the method makes use of the generalized beam-forming and forward modeling properties defined in the “CMM” algorithm. For location refinement, the method uses a stabilized version of the generalized “Geiger” approach. | 10-15-2009 |
20090271118 | Method for Obtaining Porosity and Shale Volume From Seismic Data - Method for obtaining rock parameters such as porosity and vshale directly from inversion of seismic data corresponding to a single trace location. This method is distinguished from existing methods that obtain elastic properties from inversion of seismic data, then relate the elastic parameters to rock lithology parameters such as porosity or vshale because it is accomplished in one step, can incorporate anisotropy and does not require multiple trace locations for stability. The data are separated into partial stacks, and a wavelet is specified for each stack. A set of linearized equations are constructed relating seismic reflectivity to changes in elastic parameters, and another set of linearized equations is constructed relating the changes in elastic parameters to the lithologic parameters. The linearized reflectivity equations are combined with the linearized rock physics equations, convolved with the specified wavelets, and equated to the seismic data. The resulting matrix equations are then inverted and a solution is obtained for all offsets simultaneously. | 10-29-2009 |
20090292475 | Time-Space Varying Spectra for Seismic Processing - A method and visualization apparatus for spectral analysis of time-and-space varying signals enables high resolution investigation of 3D seismic data for the exploration of oil and gas. The method extrapolates multi-resolution short windows into an average long window then computes its FFT. Extrapolation uses the continuity relationship between data inside and outside of short windows. Applications of the method are illustrated with graphical screen 3D volume displays of amplitude spectra, dip and azimuth, curvature and faults (figure below). Aside from high resolution these displays improve the productivity of a seismic interpreter. | 11-26-2009 |
20090299638 | Method for Predicting the Best and Worst in a Set of Non-Unique Solutions - Method for determining best and worst cases for values of model parameters such as porosity and shale volume fraction generated by non-unique matrix inversion of physical data such as seismic reflection amplitudes. The matrix is diagonalized, and then orthonormal basis vectors associated with insignificant diagonal elements are used to generate upper and lower bounds on the solution. Best and worst case solutions are determined as linear combinations of the null basis vectors, where the expansion coefficients are determined by making a best fit to the upper and lower bounds. | 12-03-2009 |
20090319190 | SYSTEM AND METHOD FOR SEISMIC TRACE ANALYSIS - Seismic data are processed to reduce or eliminate aliasing due, for example to sparse or irregular sampling. An iterative method includes an inhibiting function used in conjunction with a function evaluating a magnitude of Fourier coefficients that together act to reduce the effects of aliased energies and preferentially select true energies. Computational steps are conducted primarily in k-space, without returning to x-space, thereby reducing computational costs. | 12-24-2009 |
20100004869 | Vibration Isolation Device, Arithmetic Apparatus, Exposure Apparatus, and Device Manufacturing Method - An arithmetic apparatus connected to a communication net connected to a vibration isolation device. The apparatus includes a reception unit that receives seismic information via the communication net from a seismic observation device, an estimation unit that estimates seismic vibration which will arrive at the vibration isolation device, on the basis of the seismic information received by the reception unit, and a transmission unit that transmits information on the seismic vibration estimated by the estimation unit to the vibration isolation device via the communication net. | 01-07-2010 |
20100017138 | SYSTEM HAVING A NETWORK CONNECTED TO MULTIPLE DIFFERENT TYPES OF SURVEY SENSORS - A system includes a network, multiple different types of survey sensors connected to the network, and a controller connected to the network. The multiple different types of survey sensors are configured to communicate different types of measurement data over the network to the controller. | 01-21-2010 |
20100017139 | Low-power satellite-timed seismic data acquisition system - A recording system and method for conducting seismic surveys including cordless battery-operated digital recorders, each employing an integral global positioning system receiver that is only periodically enabled for the purpose of establishing synchronized acquisition clock signals among all the recorders. The satellite receiver adjustment cycle is varied depending on past acquisition clock accuracy and temperature changes. A time stamp is recorded with the digitized seismic data in non-volatile memory. The memory is sized to allow extended periods of operation. Each recorder preferably includes a low-power system timer that may be used as a timer to remotely turn on and off the recorders according to a pre-programmed schedule to conserve power when the system is not in use. Electronic components are idled or de-energized when not needed. | 01-21-2010 |
20100030478 | ANALYSIS SYSTEM, ANALYSIS METHOD, PROGRAM AND MACHINE DEVICE - According to the present invention, an analysis system constructed as a rheology model of a foundation-ground system that is capable of expressing a frequency dependent dynamic spring by using elements with non-frequency-dependent coefficients may be provided. The analysis system according to the present invention is a model for reproducing dynamical characteristics of a system including the foundation and the ground. The analysis system includes an elastic element, a damper element for damping vibration, and a reaction force generation element that generates reaction force proportional to relative acceleration of both ends thereof. The analysis system is constructed as a base system in which the elastic element, the damper element and the reaction force generation element are connected in parallel. Also, the analysis system may include at least one core system provided with any of two elements among the elastic element, the damper element and the reaction force generation element connected in parallel, and a remaining element connected serially thereto. And the base system and at least one core system may be connected in parallel to construct the analysis system. | 02-04-2010 |
20100057367 | PROCESSING SEISMIC DATA IN COMMON GROUP-CENTER GATHERS - A method for processing seismic data. The method includes plotting a travel-time curve and one or more actual times that each seismic receiver receives one or more seismograms on a graph. The travel-time curve represents an approximate time that each seismic receiver in a seismic survey area receives the seismograms. The method may further include determining a residual static shift for each seismogram and using the residual static shift to estimate a time shift correction. The residual static shift represents a difference between an actual time in which a seismic receiver received a seismogram and a time on the travel-time curve that corresponds to the actual time. The time shift correction corrects a timing error in the time indicated by the travel-time curve. | 03-04-2010 |
20100088034 | SYSTEM AND METHOD FOR DERIVING SEISMIC WAVE FIELDS USING BOTH RAY-BASED AND FINITE-ELEMENT PRINCIPLES - A system and method approximate a set of wave equations describing the propagation of seismic waves of one or more frequencies through a seismic volume of interest. In one embodiment, a ray-based initial beam solution is determined that describes the propagation of seismic waves at a first frequency through the seismic volume of interest as a set of one or more beams. Based on the ray-based initial beam solution, a refined finite-element beam solution is determined that describes the propagation of the seismic waves at the first frequency through the seismic volume of interest by approximating the two-way wave equation with a one-way wave equation. | 04-08-2010 |
20100094559 | PSEUDO LOGS TO IMPROVE STRATIGRAPHIC CORRELATION BETWEEN SEDIMENTARY BASINS - In order to improve the tie between depositionally equivalent beds relative to two or more basins detected within a multi dimensional seismic volume of interest, pseudo logs based on the average of attributes derived from seismic impedance where the compaction trend is not present are created for each basin. The mean is taken over all available azimuths, following the structural variations of introduced micro layers. The correlation between the pseudo log relative to each basin enable a more reliable interpretation between the different basins from which sound exploration decision can be made. Such a process has been successfully applied to seismic data acquired in deep water environment. | 04-15-2010 |
20100100330 | METHODS AND SYSTEMS FOR ACQUIRING AND PROCESSING SEISMIC DATA - Methods and systems are provided for acquiring seismic data. An ambient electromagnetic signal having a known time dependence is transmitted for propagation within a survey area. The ambient electromagnetic signal is received at distinct geographic locations with independently operating data acquisition units positioned at the distinct locations. Data representing acoustic signals received from the Earth at the distinct geographic locations are collected with the data acquisition units. The collected acoustic signals for the distinct geographic locations are synchronized by correlating the known time dependence of the propagated electromagnetic signal with time dependencies of the collected acoustic signals. | 04-22-2010 |
20100131205 | METHOD FOR IDENTIFYING AND ANALYZING FAULTS/FRACTURES USING REFLECTED AND DIFFRACTED WAVES - A method for fault and fracture identification based on seismic data representing a geological section using dispersion properties of reflected and diffracted waves. The method includes scanning N parameters associated with the seismic data. The array includes the coordinate axes of the angle of emergence (β), the radius of curvature of the wave front (R) and either time or depth samples. The method also includes processing the N parameters, generating a new image having a cross-sectional shape associated with one of the reflected and diffracted waves, calculating parameters DS and LS, evaluating DS for the case of fracture characterization, and comparing, for the case of fault identification, parameter LS with a threshold value defining the type of wave as one of the reflected and diffracted wave, the cross-sectional shape being substantially circular for the reflected wave, and being elliptical for the diffracted wave. | 05-27-2010 |
20100145622 | EVENT-BASED POWER MANAGEMENT FOR SEISMIC SENSORS - A method of event-based power management for seismic sensors is disclosed. The method comprises measuring seismic activity with a seismic sensor and comparing the measured seismic activity from the seismic sensor against at least one criteria. When the measured seismic activity does not satisfy the at least one criteria, a signal processing circuit is maintained in a deactivated state. When the measured seismic activity satisfies the at least one criteria, the signal processing circuit is activated to analyze the measured seismic activity. The signal processing circuit enters a functional mode based on analyzing the measured seismic activity. | 06-10-2010 |
20100161230 | Method For Predicting Differences In Subsurface Conditions - A method for predicting differences in subsurface conditions useful in 4D applications. In an example embodiment of the method, at least one layer is defined in a data volume representing a first subsurface condition such as shale volume fraction ( | 06-24-2010 |
20100174490 | Seismic Detection in Electricity Meters - An arrangement for recording seismic events includes an electricity meter sensor circuit, a digital processing circuit, and an accelerometer operably connected to the digital processing circuit. The accelerometer is configured to provide signals representative of seismic information to the digital processing circuit. A memory is configured to store data records relating to at least some of the seismic information. | 07-08-2010 |
20100211319 | RECONSTRUCTING SEISMIC WAVEFIELDS - A technique includes receiving seismic data acquired in a seismic survey in the vicinity of a reflecting interface. The survey has an associated undersampled direction. The technique includes providing second data indicative of discrete samples of incident and reflected components of a continuous seismic wavefield along the undersampled direction and relating the discrete samples to a linear combination of the continuous incident and reflected seismic wavefields using at least one linear filter. Based on the relationship, an unaliased representation of the linear combination of the continuous incident and reflected seismic wavefields is constructed. | 08-19-2010 |
20100211320 | RECONSTRUCTING A SEISMIC WAVEFIELD - A technique to reconstruct a seismic wavefield includes receiving datasets, where each dataset is indicative of samples of one of a plurality of measurements of a seismic wavefield that are associated with a seismic survey. The technique includes modeling the plurality of measurements of a seismic wavefield as being generated by the application of at least one linear filter to the seismic wavefield. The technique includes processing the datasets based on the linear filter(s) and a generalized matching pursuit technique to generate data indicative of a spatially continuous representation of the seismic wavefield. | 08-19-2010 |
20100211322 | INTERPOLATING A PRESSURE WAVEFIELD ALONG AN UNDERSAMPLED DIRECTION - A technique includes receiving seismic data acquired in a seismic survey. The survey has an associated undersampled direction, and the seismic data contains samples, which are indicative of a pressure wavefield and a directional derivative of the pressure wavefield that contains information related to vertical variations. The technique includes relating the samples to the pressure wavefield or to the directional derivative of the pressure wavefield using at least one linear filter and based on the relationship, constructing a substantially unaliased continuous representation of the pressure wavefield or the directional derivative of the pressure wavefield along the undersampled direction. | 08-19-2010 |
20100211323 | METHOD OF REPRESENTING SEISMIC SIGNALS - There is provided a method of interpolating wave signals, particularly seismic signals acquired through a seismic survey, using the steps of obtaining time series of measured wave signals; and selecting iteratively basis functions to represent said measured signals with a basis function being fully defined by n parameters, wherein in each iteration one or more basis functions are combined with the selected basis functions such that the residual between the measured signals and a representation of the measured signal by the combined basis functions is minimized at the locations of the measurement at each iteration. | 08-19-2010 |
20100211324 | AUTOMATED STRUCTURAL INTERPRETATION - Embodiments of automated structural interpretation are described. In some embodiments, a method includes identifying one or more object points belonging to an object to be tracked; tracking a trajectory of the one or more object points, including: calculating a plurality of etalons around at least one of the one or more object points using one or more different angular parameters; selecting one or more candidate points for evaluation; extracting one or more samples from around the one or more candidate points; and evaluating a next trajectory location of the one or more object points based at least partially on the one or more samples and one or more of the plurality of etalons. | 08-19-2010 |
20100235102 | TECHNIQUE AND SYSTEM TO PROCESS A SEISMIC SIGNAL TO DETERMINE AN ATTRIBUTE OF A GEOLOGICAL LAYER - A technique includes receiving seismic data indicative of a signal, which is produced by the interaction of reflection interfaces with a source wavelet. The reflection interfaces are associated with boundaries of a geological layer. The technique includes processing the seismic data to determine at least one slope change in the source wavelet caused by the interaction. The technique includes determining an attribute of the layer based at least in part on the determined slope change(s). | 09-16-2010 |
20100262372 | MICROSEISMIC EVENT MONITORING TECHNICAL FIELD - A microseismic monitoring system includes a seismic sensor positioned proximate to a wellbore traversing a formation; an orientation source producing an orientation shot; a hydraulic apparatus operationally connected with the formation to produce a fracture in the formation; a computer control system operationally connected with a database of known spectral attributes for event categories; and a computer readable medium that carries instructions executable by the computer control system that, when executed: receive data from the seismic sensor; select an event of interest from the data received; determine a spectral estimate of the selected event of interest; compare the determined spectral estimate of the selected event of interest to the known spectral estimates; and select from the data received by the seismic source the orientation shot for orientation of the seismic sensor. | 10-14-2010 |
20100274492 | DETERMINING ATTRIBUTES OF SEISMIC EVENTS - A technique includes receiving seismic data, which are acquired by a seismic sensor. The seismic data are indicative of an observed wavefield quantity that is associated with a seismic event. The technique includes determining a candidate event for an observed wavefield quantity based at least in part on a ghost model, a source wavelet and a candidate value for at least one directional attribute quantity of the seismic event; correlating the candidate event with the observed wavefield quantity; and determining an event time based on the correlating. | 10-28-2010 |
20100299069 | SPATIAL INTERPOLATION OF IRREGULARLY SPACED SEISMIC DATA - A method for spatially interpolating pressure values of seismic data uses known values of pressure and spatial derivatives of pressure at a plurality of irregularly spaced locations along the direction of interpolation. The interpolation preferably uses an interpolation operator calculated by assuming that an interpolated pressure value comprises a linear combination of the known pressure values at locations x | 11-25-2010 |
20100299070 | METHOD FOR SEPARATING INDEPENDENT SIMULTANEOUS SOURCES - This is a method of separating simultaneous sources that uses an inversion-type approach. Each source will preferably activated at a random time with respect to the others. These random delays tend to make the interference between sources incoherent while the reflections create coherent events within a series of shots. The shot separation is performed via a numerical inversion process that utilizes the sweeps for each shot, the start times of each shot, and the coherence of reflection events between nearby shots. Implementation of this method will allow seismic surveys to be acquired faster and cheaper. | 11-25-2010 |
20100318298 | IN-FIELD CONFIGURATION OF LAND SURVEY SENSORS - Described herein are implementations of various technologies for a method for in-field configuration of land survey sensors. One or more planned positions of the sensors may be received. One or more actual positions of the sensors be determined. The actual positions may be sent to the sensors while the sensors are powered off. | 12-16-2010 |
20100318299 | SYNCHRONIZING A SEISMIC DATA ACQUISITION NETWORK - Described herein are implementations of various technologies for a method for configuring a seismic data acquisition network. A first message may be received from a first node of the seismic data acquisition network over a first direct communication link. The first message may comprise a first precision quality of a first reference clock to which the first node may be synchronized. A second message may be received from a second node of the seismic data acquisition network over a second direct communication link. The second message may comprise a second precision quality of a second reference clock to which the second node may be synchronized. One of the first precision quality and the second precision quality may be determined to have a higher precision quality. A real time clock may be synchronized to one of the first reference clock and second reference clock having the higher precision quality. | 12-16-2010 |
20110022321 | METHOD FOR MONITORING A SUBTERRANEAN FRACTURE - The Invention relates to a method for monitoring a subterranean fracture, comprising determining by means of a plurality of seismic wave detectors ( | 01-27-2011 |
20110022322 | PROSPECT STRESS PREDICTION - A method is provided for obtaining a quantitative prediction of a magnitude of a maximum horizontal stress (S | 01-27-2011 |
20110035154 | UTILIZING SALTS FOR CARBON CAPTURE AND STORAGE - Aspects of the invention include methods of contacting carbon dioxide with an aqueous mixture. In practicing methods according to certain embodiments, a subterranean brine may be contacted with carbon dioxide to produce a reaction product, which may or may not be further processed as desired. Also provided are methods in which a brine or minerals are contacted with an aqueous composition. Aspects of the invention further include compositions produced by methods of the invention as well as systems for practicing methods of the invention. | 02-10-2011 |
20110046884 | SEISMIC ATTRIBUTES FOR STRUCTURAL ANALYSIS - Embodiments of methods and systems for analysis of geological structures using seismic attributes are described. In some embodiments, a method includes computing a similarity function using one or more seismic attributes at a location within the geological structure along an I direction and a J direction; computing a total optimal similarity function in at least one plane defined by the I and J directions; computing a minimum possible value of the total similarity function for a defined range of rotations; and calculating a discontinuity measure based at least partially on the minimum possible value of the total similarity function. | 02-24-2011 |
20110046885 | METHOD OF AND APPARATUS FOR EXPLORING A REGION BELOW A SURFACE OF THE EARTH - A passive method for exploring a region below the surface of the earth. The method comprises using a plurality of sensors to obtain seismic data obtained by recording ambient seismic interface waves in a frequency range whose lower limit is greater than 0 Hz, and whose upper limit is less than or equal to substantially 1 Hz. The sensors may be sensitive to three orthogonal components. Recordings may be made simultaneously by all sensors and normalization of data is unnecessary. The sensors may be moved and clean data may be selected. Local dispersion curves may be determined to improve vertical resolution. The data are processed so as to obtain a measure of the energy in a frequency band within the frequency range. The energy measure may be calculated by integrating the spectrum in the frequency domain over a desired frequency range. The resulting calculated energy provides information about the region of the earth being explored. | 02-24-2011 |
20110082645 | VARIABLE GRID FOR FINITE DIFFERENCE COMPUTATION - A computer system and a computer-implemented method for evaluating a geophysical model using a grid of points representing locations in a subsurface geological region are disclosed. The method includes storing a geophysical model of the subsurface geological region in a computer readable memory and defining, for the geophysical model, the grid of points representing the locations in the subsurface geological region. The grid of points comprise a plurality of points extending in at least one direction. The plurality of points are variably spaced apart in the at least one direction. The method further includes evaluating, by the computer, the geophysical model using the grid of points. | 04-07-2011 |
20110093202 | SYSTEMS AND METHODS FOR MONITORING AND DETECTING AN EVENT - A system for monitoring and detecting an event. A position determining unit configured to receive a position determining signal. A seismic event detector configured to detect a seismic event and generate a seismic event signal. A storage unit configured for storing position information corresponding to the position determining signal, the storage of the position information occurs in a first manner. A storage unit manager configured to alter the first manner of the storing the position information upon a receipt of the seismic event signal. | 04-21-2011 |
20110098932 | METHOD AND APPARATUS FOR DETECTING PEDESTRIANS - Detection of at least one object causing a signal of interest. In one embodiment, a method of detecting at least one object causing a persistent non-random pressure wave comprises: providing a digital signal representation of the pressure wave that includes respective amplitudes of the signal, in at least two different frequencies, and providing a detection indication based on a measured similarity between the respective amplitudes over time. | 04-28-2011 |
20110118984 | METHOD AND SYSTEM FOR RETRIEVING SEISMIC DATA FROM A SEISMIC SECTION IN BITMAP FORMAT - A computer implemented method for retrieving seismic data from a seismic section provided in a bitmap format. The method includes reconstructing a two dimensional matrix of seismic interpolated data in which a value at a given pixel in the matrix is proportional to local density of wiggles in the seismic section with an added value of a previously calculated pixel. The method may be implemented in either of computer hardware configured to perform said method and computer software embodied in a non-transitory, tangible, computer-readable storage medium. Also disclosed are corresponding computer program product and data processing system. | 05-19-2011 |
20110125406 | SYSTEM AND METHOD FOR ATTENUATING MULTIPLES IN SEISMIC DATA THAT ACCOUNTS FOR BEAM AZIMUTH - The present invention incorporates the use of model-driven and data-driven methodologies to attenuate multiples in seismic data utilizing a prediction model which includes multiply-reflected, surface-related seismic waves. The present invention includes beam techniques that account for beam azimuth, and convolving a predicted multiples beam with a segment of a modeled pegleg beam to obtain a convolved multiples beam. The convolved multiples beam can then be deconvolved to attenuate the multiples that are present in the original input beam. | 05-26-2011 |
20110125407 | Apparatus and Method for Integrating Survey Parameters into a Header - A method, apparatus and system for acquiring seismic data is disclosed that in one aspect receives a seismic signal detected by at least one sensor in response to a seismic energy signal generated by a source at a selected location at a data acquisition unit in data that is in data communication with the sensor, receives at least one parameter of the source and/or receiver at the data acquisition unit; and generates a data block at the data acquisition unit having data representative of the received seismic signal and a header that contains data representative of the at least one parameter of the source and/or receiver. It is emphasized that this abstract is provided to comply with the rules requiring an abstract which will allow a searcher or other reader to quickly ascertain the subject matter of the technical disclosure. It is submitted with the understanding that it will not be used to interpret or limit the scope or meaning of the claims. | 05-26-2011 |
20110191032 | INTERPOLATION OF PERIODIC DATA - A method for interpolating data. The method includes receiving data acquired at one or more locations where the data represents subterranean formations in the earth. The method also includes selecting one or more of the locations such that the selected locations are within a vicinity of an interpolation location. Next, the method includes forming a matrix of interpolation coefficients based on a first function having one or more interpolation variables, a bandwidth for an interpolation operator and one or more differences between the selected locations, wherein at least one of the interpolation variables is periodic. The method then includes forming a differences vector based on a second function having the interpolation variables, the bandwidth and one or more differences between the selected locations and the interpolation location. Using the matrix of interpolation coefficients and the differences vector, the method then forms an interpolation operator vector by applying an inverse of the matrix of interpolation coefficients to the differences vector. The method then estimates a data value for the interpolation location using the interpolation operator vector. | 08-04-2011 |
20110196613 | METHOD OF CHARACTERIZING A CO2 PLUME IN A GEOLOGICAL STORAGE AQUIFER - A method of monitoring a CO | 08-11-2011 |
20110202278 | MULTI-FUNCTION BROADBAND PHASED-ARRAY SOFTWARE DEFINED SONAR SYSTEM AND METHOD - A software defined platform is provided for subsea acoustic applications that utilizes a broadband phased array transducer and a configurable, multi-function software defined transducer that is configurable on the fly to enable various subsea acoustic systems to be achieved in a single unit thus reducing the space required on the vessel and the cost of having such multiple functions. | 08-18-2011 |
20110213556 | SYSTEM AND METHOD FOR LOCAL ATTRIBUTE MATCHING IN SEISMIC PROCESSING - There is provided herein a New system arid method of local attribute match filtering which operates in the local attribute domain via the use of complex wavelet transform technology. This approach is adaptable to address various noise types in seismic data and, more particularly, is well suited to reduce the noise in geophone data as long as an associated hydrophone signal is relatively noise-free. | 09-01-2011 |
20110231100 | ROTATIONAL SEISMOMETER FOR NEAR-FIELD MEASUREMENTS - A rotational seismometer having a housing that encases an optical lever having a light source for emitting a beam of light through a slit defined by the optical lever that is focused by a lens for focusing the beam of light to a balance bob suspended within the housing is disclosed. The balance bob includes a mirror secured to a plate attached to the housing through an arrangement that includes a thin fiber attached to a stiff wire such that the stiff wire bends and the thin wire does not bend when a tilt motion is applied to the rotational seismometer. | 09-22-2011 |
20110251797 | METHOD OF MONITORING A GEOLOGICAL GAS STORAGE SITE BY STRATIGRAPHIC INVERSION OF SEISMIC DATA - A method of monitoring an underground formation into which a gas is injected or from which a gas is produced, by a stratigraphic inversion of seismic data with anamorphosis of impedances. Pre-injection and post-injection seismic data are acquired. A pre-injection seismic impedance cube IP | 10-13-2011 |
20110313671 | SYSTEM AND METHOD FOR DETECTING ROCK FALL - Aspects of the invention provide systems and methods for using ballast sensors to detect rock fall events in a vicinity of railway tracks or similar roadways or tracks. The ballast sensors are spaced apart from the tracks. Particular embodiments permit the use of signals from the ballast sensors to discriminate rock fall events from other types of events and to detect the hypocenter of a rock fall event. | 12-22-2011 |
20110320129 | SHOT GATHER DATA BEAMER AND DEBEAMER - Beamed data can be obtained from shot gather data, and debeamed data can be obtained from beamed data. Shot gather data for a geophysical volume of interest in a first domain and/or beamed data in a third domain may be received. The first domain has a component relating to seismic wave propagation time and a spatial component relating to lateral spacing. The third domain has a component relating to local plane wave arrival time at a beam center surface location and a component relating to plane wave arrival directions. Data may be transformed between the first domain and a second domain. The second domain has a frequency component and a spatial component corresponding to the spatial component of the first domain. Data may be weighted and/or deweighted in the second domain using a weighting function. A forward transform may be applied to weighted shot gather data in the first domain to obtain beamed data in the third domain. A reverse transform may be applied to beamed data in the third domain to obtain weighted debeamed data in the first domain. | 12-29-2011 |
20120004849 | EFFICIENT WINDOWED RADON TRANSFORM - One or more computer-readable media including computer-executable instructions to instruct a computing system to define a Radon transform convolution mask; specify an angle that defines a line extending at least partially across a pixel image; and apply the mask successively to target pixels on the line to compute a statistical value for each of the target pixels where application of the mask identifies a set of pixels for computing the statistical value and where each successive application of the mask identifies a set of pixels that includes at least one pixel of a prior set and at least one pixel not included in the prior set to thereby reduce requirements for computing the statistical values. Various other apparatuses, systems, methods, etc., are also disclosed. | 01-05-2012 |
20120004850 | SYSTEM AND METHOD FOR MIGRATING SEISMIC DATA - A system and method that enable the processing of seismic data. In one embodiment, a system comprises a plurality of processing nodes and a server. The plurality of processing nodes are configured to process seismic data for migration. The server is operatively linked to each of the plurality of processing nodes to enable communication between the server and the processing nodes. The server may manage a set of stored beam tables that can be accessed by the processing nodes in order to process seismic data. | 01-05-2012 |
20120035852 | PROCESSING SEISMIC DATA - A method of processing multi-component seismic data is provided that comprises determining, in the time-offset domain, a first partition rate for a first event from the multi-component seismic data. Information about near-receiver properties of the earth may be obtained from the first partition rate. The method may further comprise determining, in the time-offset domain, at least a second partition rate for the first event from the multi-component seismic data and/or at least a third partition rate for a second event. Further information about near-receiver properties of the earth can be obtained from the second and/or third partition rate. | 02-09-2012 |
20120072115 | DETERMINATION OF NOTIONAL SIGNATURES - A method of determining the signature of a seismic source array comprises determining a notional signature of at least one source of an array of n seismic sources from measurements of the emitted wavefield from the array made at 2n independent locations and from the relative positions of the sources of the array and the 2n independent locations. The notional signature of a source may be determined from the difference (or some other function) of the measurements of the emitted wavefield made by the two sensors associated with that source. | 03-22-2012 |
20120072116 | EXTRACTION OF DEPOSITIONAL SYSTEMS - A process that assists with the identification of potential hydrocarbon deposits that includes performing a structural interpretation of a three-dimensional seismic volume, transforming the three-dimensional seismic volume into a stratal-slice volume, performing a stratigraphic interpretation of the stratal-slice volume which includes the extracting of bounding surfaces and faults and transforming the stratal-slice volume into the spatial domain. As illustrated in FIGS. | 03-22-2012 |
20120095689 | PROCESSING SEISMIC DATA - A method of processing seismic data acquired consequent to actuation of a seismic source is described. The method comprises taking the result of the following process into account when processing the seismic data where the process comprises estimating the effect of uncertainty in the position and/or orientation of the seismic source relative to the measuring receiver on processing the seismic data by estimating a source wavefield from data acquired by a near-field measuring receiver and from a first parameter set including at least one parameter indicative of the position and/or orientation of the seismic source relative to the measuring receiver, varying the value of at least one parameter of the first parameter set, estimating the source wavefield from the data acquired by the measuring receiver and from the varied first parameter set and obtaining information about the uncertainty in the estimate of the source wavefield. | 04-19-2012 |
20120123684 | SYSTEM AND METHOD FOR GENERATING MICRO-SEISMIC EVENTS AND CHARACTERIZING PROPERTIES OF A MEDIUM WITH NON-LINEAR ACOUSTIC INTERACTIONS - A method and system includes generating a first coded acoustic signal including pulses each having a modulated signal at a central frequency; and a second coded acoustic signal each pulse of which includes a modulated signal a central frequency of which is a fraction d of the central frequency of the modulated signal for the corresponding pulse in the first plurality of pulses. A receiver detects a third signal generated by a non-linear mixing process in the mixing zone and the signal is processed to extract the third signal to obtain an emulated micro-seismic event signal occurring at the mixing zone; and to characterize properties of the medium or creating a 3D image of the properties of the medium, or both, based on the emulated micro-seismic event signal. | 05-17-2012 |
20120130643 | IDENTIFYING INVALID SEISMIC DATA - A method for processing seismic data. The method may include (1) receiving seismic data acquired by an i | 05-24-2012 |
20120130644 | ELECTRICAL METHODS SEISMIC INTERFACE BOX - The present invention relates to a method and apparatus for evaluating the geometry of a fracture. | 05-24-2012 |
20120173150 | SENSOR-BASED SYSTEMS AND METHODS FOR ASSESSING INTERNAL BRIDGE DECK DETERIORATION - An interior volume of a bridge deck is probed using a transportable sensor system that produces deck data useful for assessing internal degradation of the bridge deck. Geographic position data of sensor system positioning is produced as the sensor system traverses the deck. The deck data is associated with the one or more deck locations using the geographic positioning data, and adjusted deck data is generated using adjustment data indicative of external factors that influence the deck data but are unrelated to a failure mechanism impacting the bridge deck interior. An output may be generated comprising at least the adjusted deck data. | 07-05-2012 |
20120197530 | EXTRACTING GEOLOGIC INFORMATION FROM MULTIPLE OFFSET STACKS AND/OR ANGLE STACKS - Geologic information may be extracted from multiple offset stacks and/or angle stacks. Offset stacks and/or angle stacks may be received that represent energy that has propagated through a geologic volume of interest from energy sources to energy receivers. Attribute volumes associated with individual source-receiver offsets and/or source-receiver angles may be determined based on corresponding offset stacks and/or angle stacks. For individual offset stacks or angle stacks, corresponding sets of geologic features represented in the attribute volumes may be identified. The sets of geologic features corresponding to the different offset stacks and/or angle stacks to may be compared to determine discrepancies and/or similarities between the sets of geologic features corresponding to the different offset stacks and/or angle stacks. Stratigraphic interpretations, stratigraphic predictions, and/or other interpretations and/or predictions may be determined based on causes of the discrepancies and/or similarities. | 08-02-2012 |
20120197531 | EXTRACTING GEOLOGIC INFORMATION FROM MULTIPLE OFFSET STACKS AND/OR ANGLE STACKS - Geologic information may be extracted from multiple offset stacks and/or angle stacks. Offset stacks and/or angle stacks may be received that represent energy that has propagated through a geologic volume of interest from energy sources to energy receivers. Attribute volumes associated with individual source-receiver offsets and/or source-receiver angles may be determined based on corresponding offset stacks and/or angle stacks. For individual offset stacks or angle stacks, corresponding sets of geologic features represented in the attribute volumes may be identified. The sets of geologic features corresponding to the different offset stacks and/or angle stacks to may be compared to determine discrepancies and/or similarities between the sets of geologic features corresponding to the different offset stacks and/or angle stacks. Stratigraphic interpretations, stratigraphic predictions, and/or other interpretations and/or predictions may be determined based on causes of the discrepancies and/or similarities. | 08-02-2012 |
20120197532 | EXTRACTING GEOLOGIC INFORMATION FROM MULTIPLE OFFSET STACKS AND/OR ANGLE STACKS - Geologic information may be extracted from multiple offset stacks and/or angle stacks. Offset stacks and/or angle stacks may be received that represent energy that has propagated through a geologic volume of interest from energy sources to energy receivers. Attribute volumes associated with individual source-receiver offsets and/or source-receiver angles may be determined based on corresponding offset stacks and/or angle stacks. For individual offset stacks or angle stacks, corresponding sets of geologic features represented in the attribute volumes may be identified. The sets of geologic features corresponding to the different offset stacks and/or angle stacks to may be compared to determine discrepancies and/or similarities between the sets of geologic features corresponding to the different offset stacks and/or angle stacks. Stratigraphic interpretations, stratigraphic predictions, and/or other interpretations and/or predictions may be determined based on causes of the discrepancies and/or similarities. | 08-02-2012 |
20120209530 | INTERBED MULTIPLE PREDICTION - A method and apparatus for predicting interbed multiples is described herein. Trace geometries may be generated for one or more desired shot-side traces, one or more desired receiver-side traces, and one or more desired interbed multiple generator traces, for a first target trace. A first set of reflections at the interbed multiple generator layer may be extracted from one or more recorded traces closest to the desired interbed multiple generator traces. A second set of reflections below the interbed multiple generator layer may be extracted from one or more recorded traces closest to the desired shot-side traces. A third set of reflections below the interbed multiple generator layer may be extracted from one or more recorded traces closest to the desired receiver-side traces. The interbed multiples for the first target trace may be estimated based on the first set, the second set, and the third set. | 08-16-2012 |
20120253681 | SYSTEM AND METHOD FOR PROCESSING SEISMIC DATA - A computer-implemented method for processing seismic data includes the determining, from the seismic data, a first amplitude attribute map at a first image depth corresponding to a shallow attenuating body, and a second amplitude attribute map at a second image or target depth. The first and second amplitude attribute maps are then normalized, and a ratio map is determined based on a ratio of the normalized first and second amplitude attribute maps. The ratio map is scaled to yield a scale factor map, which is then applied to the seismic data to compensate for effects of shallow overburden attenuation. | 10-04-2012 |
20120265445 | STABLE SHOT ILLUMINATION COMPENSATION - Various embodiments provide a system and a shot illumination compensation method implemented on a computer system for imaging a subsurface formation. The method includes receiving, by the computer system, seismic data produced by an acoustic energy source and reflected by the subsurface formation; and generating, by the computer system, an image of the subsurface formation based on the seismic data and a spatially varying damping parameter. | 10-18-2012 |
20120283953 | LINE AND EDGE DETECTION AND ENHANCEMENT - Embodiments of the present disclosure include one or more of a method, computing device, computer-readable medium, and system for statistical line and edge detection and/or enhancement. An example embodiment of the present disclosure may include a method that includes identifying a plurality of data values related to a first object defined by a first plurality of points within the volume, wherein the first object intersects a second object defined by a second plurality of points within the volume; calculating a statistical significance statistic related to the second object; interpolating a P-value related to the statistical significance statistic; and determining a significant P-value taken over the second object, wherein the significant P-value comprises a minimum P-value that provides a maximum negative log(P(statistical significance statistic)). | 11-08-2012 |
20120316790 | SYSTEM AND METHOD FOR DATA INVERSION WITH PHASE EXTRAPOLATION - A system and computer-implemented method for inverting data from an area of interest to determine physical properties of the area of interest is disclosed. The method includes transforming the data into a Fourier frequency domain to obtain frequency domain data wherein the frequency domain data includes an amplitude portion and a phase portion, performing phase unwrapping of the phase portion of the frequency domain data to generate an unwrapped phase portion of unwrapped data, extrapolating the unwrapped phase portion to create extrapolated unwrapped data, and inverting the extrapolated unwrapped data to determine the physical properties of the area of interest. The data inverted may be, for example, seismic data or synthetic aperture radar data. The system includes a data source, an user interface, and a processor configured to execute computer modules designed to implement the method. | 12-13-2012 |
20120316791 | SYSTEM AND METHOD FOR SEISMIC DATA INVERSION BY NON-LINEAR MODEL UPDATE - A system and computer-implemented method for determining properties of a subsurface region of interest from seismic data is disclosed. An embodiment of the method performs full waveform inversion by non-linear model update to compute a velocity model. The method includes obtaining actual seismic data representative of the subsurface region and an initial earth property model for the subsurface region, performing forward modeling using the initial earth property model to create modeled seismic data with similar acquisition specifications as the actual seismic data, calculating a residual between the actual seismic data and the modeled seismic data in a time or transform domain, and inverting the residual to generate a model produced by non-linear model update components. The system includes a data source, user interface, and processor configured to execute computer modules that implement the method. | 12-13-2012 |
20130013212 | SEISMIC CLOCK TIMING CORRECTION USING OCEAN ACOUSTIC WAVES - A method for identifying clock timing discrepancies in at least one clock of interest that is associated with a marine seismic receiver, comprises collecting from at least one marine receiver other than the receiver of interest a first data set corresponding to a selected time period, said first data set being selected to include ocean wave signals; collecting from the receiver of interest a second data set corresponding to the selected time period, said second data set being selected to include ocean wave signals; applying a mathematical prediction technique to the ocean wave signals in the first data set so as to generate a predicted response for a receiver co-located with the receiver of interest; comparing the predicted response to the second data set so as to generate a correlation data set; and using the correlation data set to determine a corrected parameter for the receiver of interest. | 01-10-2013 |
20130041589 | PASSIVE MONITORING METHOD FOR SEISMIC EVENTS - The invention concerns a passive monitoring method to detect the presence of and characterize a micro-seismic event ( | 02-14-2013 |
20130054147 | System and Method for Narrow Beam Scanning Microseismic Monitoring - Disclosed herein are various embodiments of methods and systems for optimizing signals generated by microseismic sources, comprising recording microseismic data using patches of geophones, filtering the data to impart a directionality to the data, and performing a source scan to determine the times and locations of microseismic events. The subsurface is divided into a voxel grid that is further subdivided into subgrids. Using a filter designed for each patch-subgrid pair, only data arriving within a predetermined angle of incidence are input to the source scan, thus reducing noise, and enhancing the quality and accuracy of the identified microseismic events. The method is also applicable to data previously recorded with sensor grids or other arrays such as star arrays. | 02-28-2013 |
20130060476 | PROCESSING GEOPHYSICAL DATA - The present invention relates to a method of processing seismic data and other geophysical data such as acoustic or electromagnetic data. In particular the method is applicable to seismic data extrapolation and migration techniques such as, for example, one-way and two-way wave-equation migration. The method comprises determining, in the space-time domain, an integral of the product of a kernel and a function of the geophysical data over an integration domain from the values of the function at a plurality of discrete data points within the integration domain by defining a plurality of cells in the integration domain, each vertex of a cell being at a respective one of the data points; obtaining an interpolant of the function over a selected cell using local interpolation; and integrating, in the space-time domain, the product of the kernel and the interpolant for the selected cell. | 03-07-2013 |
20130090857 | Tensor-Based Method For Representation, Analysis, and Reconstruction of Seismic Data - Method for representing seismic data as a spatially varying, second-order tensor field ( | 04-11-2013 |
20130090858 | SYSTEM FOR MEASURING COSEISMIC MOVEMENTS OR VIBRATIONS OF STRUCTURES BASED ON GLOBAL NAVIGATION SATELLITE SYSTEMS-GNSS AND/OR PSEUDOLITES - System for measuring coseismic movements or vibrations of structures based on measurements of phase observations performed on at least four sources simultaneously, between GNSS satellites and/or pseudolites, for couples of consecutive timepoints (t,t+1) temporally separated by not more than one second. | 04-11-2013 |
20130151161 | Seismic Horizon Skeletonization - Method for analysis of hydrocarbon potential of subterranean regions by generating surfaces or geobodies and analyzing them for hydrocarbon indications. Reflection-based surfaces may be automatically created in a topologically consistent manner where individual surfaces do not overlap themselves and sets of multiple surfaces are consistent with stratigraphic superposition principles. Initial surfaces are picked from the seismic data ( | 06-13-2013 |
20130158877 | Processing of Geological Data - A method of processing data points distributed throughout a geological volume is described. In the method, each data point is associated with respective geological attributes. The method provides for: coding the geological attributes of each data point as a respective character string; compiling a query character string defining sought geological attributes of an arrangement of one or more data points; searching the coded geological attributes for arrangements of data points having geological attributes matching the query character string; and identifying matched data points. | 06-20-2013 |
20130158878 | DEVICE AND METHOD FOR LOCATING MICROSEISMIC EVENTS USING ARRAY OF RECEIVERS - Device and method for locating a microseismic event taking place in a subsurface of the earth. The method includes receiving recorded seismic data S(t, Rc) acquired by a plurality of receivers as a function of time t and a position Rc; receiving a reference signal model SiMo(t, Rc) that corresponds to seismic data recorded by the plurality of receivers if an explosion occurs at an injection point in the subsurface; time correlating the recorded seismic data S(t, Rc) with the signal model SiMo(t, Rc) to determine correlated seismic data DMSS; calculating a detection curve for each of plural cells in a given volume in the subsurface of the earth based on the correlated seismic data DMSS; and determining a seismic location in the volume of the microseismic event based on a largest value of maximums of the detection curves calculated for various points of the given volume in the subsurface. | 06-20-2013 |
20130191031 | HIGH-PRECISION TIME SYNCHRONIZATION FOR A CABLED NETWORK IN LINEAR TOPOLOGY - The present disclosure relates to methods and apparatuses for reducing propagation delay uncertainty while conducting a survey. The apparatus includes a plurality of nodes along a communication path configured to allow communication between nodes with only one clock domain boundary crossing. Each node may include a clock, a memory, and a processor. The plurality of nodes is arranged in a linear topology. The linear topology may have first and second nodes on the ends of the line. The method may include reducing propagation delay uncertainty using at least one time marker transmitted to each of the plurality of nodes without crossing a clock domain boundary of any other node. | 07-25-2013 |
20130211726 | DETECTING BROADSIDE AND DIRECTIONAL ACOUSTIC SIGNALS WITH A FIBER OPTICAL DISTRIBUTED ACOUSTIC SENSING (DAS) ASSEMBLY - A Distributed Acoustic Sensing (DAS) fiber optical assembly comprises adjacent lengths of optical fiber A, B with different directional acoustic sensitivities, for example by providing the first length of optical fiber A with a first coating 35, such as acrylate, and the second length of optical fiber B with a second coating | 08-15-2013 |
20130211727 | Method to Improve Spatial Sampling of Vertical Motion of Seismic Wavefields on the Free Surface of the Earth by Utilizing Horizontal Rotational Motion and Vertical Motion Sensors - The present method provides spatial sampling of a seismic wavefield on the free surface of the earth at an effective spatial sampling denser than the physical layout of the sensors. The sensors are comprised of a sensing element for vertical particle motion at the earth's surface, and a sensing element for rotational motion around a horizontal axis at the surface of the earth. Stress and wavefield conditions known at the free surface of the earth allow the rotational sensing element to yield the transverse horizontal gradient of the vertical particle motion wavefield. This horizontal gradient and the vertical particle motion data are utilized in the technique of ordinate and slope sampling to yield an improved transverse spatial sampling of the vertical particle motion wavefield. The method has a wide range of application in seismic surveys in oil and gas exploration and production. | 08-15-2013 |
20130238246 | Orthogonal Source and Receiver Encoding - Method for performing simultaneous encoded-source inversion of geophysical data to estimate parameters of a physical property model ( | 09-12-2013 |
20130238247 | METHODS OF HYDROCARBON DETECTION USING SPECTRA DOMINANT FREQUENCY AND MEASURES OF ENERGY DECAY ON THE LOW SIDE AND HIGH SIDE OF SPECTRA DOMINANT FREQUENCY - A method for detecting hydrocarbons including obtaining seismic trace data for a region of interest; processing, using a processor, the seismic trace data to calculate a signal spectrum for each of a plurality of locations in the region of interest; calculating a dominant frequency of the signal spectrum; calculating at least one measure of energy decay above the dominant frequency, calculating at least one measure of energy decay below the dominant frequency, and calculating at least one measure spectral shape of the signal spectrum, and locating a hydrocarbon reservoir in the region of interest using the at least one measure of energy decay below the dominant frequency, the at least one measure of energy decay above dominant frequency and the dominant frequency; or locating a hydrocarbon reservoir in the region of interest using the at least one measure of energy decay below the dominant frequency and the at least one measure of energy decay above dominant frequency; or and locating a hydrocarbon reservoir in the region of interest using the at least one measure of energy decay below the dominant frequency and the dominant frequency; or locating a hydrocarbon reservoir in the region of interest using the at least one measure of spectral shape and the dominant frequency. | 09-12-2013 |
20130245954 | SEISMIC IMAGING SYSTEM USING COSINE TRANSFORM IN LOGARITHMIC AXIS - Provided is seismic imaging, particularly, a seismic imaging system. The seismic imaging system includes a measured data processing unit converting measured data from receiver to cosine transformed data in logarithmic scale axes, a subsurface structure estimating unit calculating subsurface modeling parameters with measured data transformed in the measured data processing unit based on a cosine transformed acoustic waveform equation defined along logarithmic axes, and an image output unit converting modeling parameters calculated in the subsurface structure estimating unit and outputting the converted image data. | 09-19-2013 |
20130245955 | CORRECTING GEOMETRY-RELATED TIME AND AMPLITUDE ERRORS - A method for predicting a plurality of surface multiples for a plurality of target traces in a record of seismic data acquired in a survey area. The method includes selecting a target trace and identifying two or more desired traces for multiple prediction based on the target trace. After identifying the desired traces, the method identifies one or more recorded traces for each desired trace. Each identified recorded trace is described as being substantially close to one of the desired traces. The method then includes correcting the identified recorded traces for one or more geometry-related effects associated with the survey area and convolving the corrected recorded traces to generate a plurality of convolutions. After convolving the corrected recorded traces, the method then stacks the convolutions. | 09-19-2013 |
20130261980 | USING CROSSLINE MEASUREMENT DATA FOR AN ACTION RELATING TO SURVEY OF A TARGET STRUCTURE - Methods and systems for survey operations are provided. In some embodiments, crossline measurement data measured by at least one survey receiver is received. Based at least in part on a characteristic of the crossline measurement data, an option from among a plurality of candidate options is selected, where the selected option is for use in an action relating to survey of a target structure. | 10-03-2013 |
20130261981 | COVARIANCE ESTIMATION USING SPARSE WAVELET REPRESENTATION - Computing systems and methods are disclosed. In one embodiment, a technique is provided that includes receiving data representing at least in part a structure of interest; and processing the data in a processor-based machine to represent the data as a data structure including a plurality of contiguous data segments and at least one disjoint section, which separates two of the contiguous data segments. The technique includes processing the data structure based at least in part on the disjoint section(s) exhibiting ergodic behavior to determine at least one property of the structure. | 10-03-2013 |
20130338927 | Seismic Anomaly Detection Using Double-Windowed Statistical Analysis - Method for identifying geologic features from seismic data ( | 12-19-2013 |
20130345985 | SEISMIC ORTHOGONAL DECOMPOSITION ATTRIBUTE - A method can include providing seismic data for a subsurface region that includes a reflector; decomposing at least a portion of the seismic data using principal component analysis (PCA) to generate at least one principal component; and outputting output data based at least in part on the at least one principal component. Various other apparatuses, systems, methods, etc., are also disclosed. | 12-26-2013 |
20140019055 | SYSTEM AND METHOD FOR ESTIMATING AND ATTENUATING NOISE IN SEISMIC DATA - A system and method for attenuating noise in seismic data representative of a subsurface region of interest including receiving the seismic data; transforming the seismic data into a domain wherein the seismic data have a sparse or compressible representation to create transformed seismic data; dividing the domain into windows wherein the windows represent known spatio-temporal locations in the seismic data; determining statistics of the transformed seismic data in each window; determining a filter for each window based on the statistics of the transformed data; applying the filter for each window to the transformed seismic data in each window to create filtered seismic data; and performing an inverse transform of the filtered seismic data to create noise-attenuated seismic data. | 01-16-2014 |
20140019056 | PROCESS FOR CHARACTERISING THE EVOLUTION OF AN OIL OR GAS RESERVOIR OVER TIME - Disclosed is a process for characterising the evolution of a reservoir that comprises non-horizontal layers, by analyzing the changes of at least the seismic amplitudes of seismic reflections. The process comprises the steps of providing a base survey of the reservoir with a set of seismic traces at a first time and providing a monitor survey of the reservoir, taken at a second time, with a set of seismic traces associated to the same positions as in the base survey. The sets of seismic traces from the base and monitor surveys are then inverted to obtain an estimate of the changes having occurred in the time interval between base and monitor surveys, the inversion being performed using seismic traces for which allowance is made for the actual propagation paths through the non-horizontal layers of the reservoir. | 01-16-2014 |
20140025304 | INVERTED SEISMIC ATTRIBUTE QUALITY AND LOCAL ROCK PHYSICS CALIBRATION - Methods and processing in the field of seismic data, particularly to more accurately predict petrophysical property variables at unsampled locations beyond and between wells. | 01-23-2014 |
20140032119 | METHOD OF ANALYZING SEISMIC DATA - Post-migration common image gathers (CIGs) are generated in a dip angle domain from measured seismic data. From a CIG, a hybrid Radon model is determined, including a reflection model related to concave features in the CIG and a diffraction model related to linear features in the CIG. The reflection model is transformed with a reflection Radon operator applied along inversion trajectories restricted around apices of the concave features to obtain reflection data. The diffraction model is transformed with a diffraction Radon operator to obtain diffraction data. The reflection and diffraction data at different horizontal positions can then be combined and summed to generate a migrated image of the subsurface. | 01-30-2014 |
20140039798 | SYSTEM AND METHODS FOR GROUPING SIMILAR ITEMS WITHIN A SET - A system is disclosed comprising a non-transitory, computer-readable storage device storing software. The software, when executed by a processor, causes the processor to perform the following operations for each of a plurality of non-functional electronic devices: count a number of other non-functional electronic devices within a defined distance from the non-functional electronic device; and define the non-functional electronic device to be a core electronic device if the counted number is at least a threshold value, wherein threshold value is based on a total number of electronic devices within the defined distance around the non-functional electronic device. For each core electronic device, the software, when executed by a processor, further causes the processor to form a neighborhood group comprising the core electronic device and other non-functional electronic devices within the defined distance around the core electronic device. | 02-06-2014 |
20140039799 | Seismic Inversion for Formation Properties and Attentuation Effects - Method for inverting seismic data to obtain reflection properties by estimating or measuring ( | 02-06-2014 |
20140046599 | SYSTEM AND METHOD OF A RESERVOIR MONITORING SYSTEM - Reservoir monitoring system. At least some of the illustrative embodiments are methods comprising installing a hydrocarbon reservoir monitoring system in a marine environment. The installing may be by: placing a base unit at the sea floor, the base unit communicatively coupled to a computer system at the surface, the communicative coupling by way of an umbilical cable; mechanically coupling a first termination module to the base unit, the termination module coupled to a first sensor cable; and communicatively coupling the first sensor cable to the umbilical cable. | 02-13-2014 |
20140058678 | True-Amplitude Layer-Stripping in Fractured Media - Method for determining fracture orientation and fracture intensity in multiple fractured layers in the subsurface in a layer-stripping manner. Multi-component, multi-azimuth seismic data are required ( | 02-27-2014 |
20140067273 | System and method for constrained least-squares spectral processing and analysis of seismic data - An inversion-based algorithm for computing the time frequency analysis of reflection seismograms using constrained least-squares spectral analysis is formulated and applied to modeled seismic waveforms and real seismic data. The Fourier series coefficients are computed as a function of time directly by inverting a basis of truncated sinusoidal kernels for a moving time window. Spectra may be provided that have reduced window smearing for a given window length relative to the discrete Fourier transform irrespective of window shape, and a time-frequency analysis with a combination of time and frequency resolution that is superior to the short time Fourier transform and the continuous wavelet transform. The reduction in spectral smoothing enables enhanced determination of spectral characteristics of interfering reflections within a short window. The degree of resolution improvement relative to the short time Fourier transform increases as window length decreases. | 03-06-2014 |
20140081576 | MIXED SEQUENTIAL AND SIMULTANEOUS SOURCE ACQUISITION AND SYSTEM - Systems and methods for acquiring blended and unblended seismic data during a single seismic survey. The blended and unblended seismic data is generated with a plurality of sources that are fired in a dedicated sequence. The sequence involves firing all the sources at a first time, advancing the sources along a given path, firing only a first source at a second time, later than the first time, advancing the sources, firing again all the sources at a third time, later than the second time, advancing the sources, firing only a second source at a fourth time, later than the third time, and so on until a desired subsurface is fully surveyed. | 03-20-2014 |
20140107930 | PLURAL DEPTH SEISMIC SOURCE SPREAD METHOD AND SYSTEM - A method for acquiring and improving seismic data includes activating a first seismic source located below a geophysical surface at a first depth and a second seismic source located below the geophysical surface at a second depth, wherein the second depth is below the first depth, acquiring seismic data with a seismic receiver in conjunction with activating the first seismic source and the second seismic source, and aligning primary reflections within the seismic data to provide improved seismic data. The method may also include determining changes to the regions below the second depth by comparing improved seismic data corresponding to a first acquisition event with improved seismic data corresponding to a second acquisition event. A corresponding system is also disclosed herein. | 04-17-2014 |
20140142858 | LOW-POWER SATELLITE-TIMED SEISMIC DATA ACQUISITION SYSTEM - A recording system and method for conducting seismic surveys including cordless battery-operated digital recorders, each employing an integral global positioning system receiver that is only periodically enabled for the purpose of establishing synchronized acquisition clock signals among all the recorders. The satellite receiver adjustment cycle is varied depending on past acquisition clock accuracy and temperature changes. A time stamp is recorded with the digitized seismic data in non-volatile memory. The memory is sized to allow extended periods of operation. Each recorder preferably includes a low-power system timer that may be used as a timer to remotely turn on and off the recorders according to a pre-programmed schedule to conserve power when the system is not in use. Electronic components are idled or de-energized when not needed. | 05-22-2014 |
20140149045 | SYSTEM AND METHOD FOR DEDUCING CAVERN PROPERTIES - Strength parameters of the contents of subsurface caverns are deduced through seismic information. Known properties of formations surrounding the caverns, and ratios of seismic amplitudes between the caverns and the surrounding formations are leveraged to deduce the strength parameters within the caverns | 05-29-2014 |
20140149046 | METHOD OF PROCESSING SEISMIC DATA BY PROVIDING SURFACE OFFSET COMMON IMAGE GATHERS - The method processes input including, for each of a plurality of shots at respective source locations, seismic traces recorded at a plurality of receiver locations. Offset-modulated data are also computed by multiplying the seismic data in each seismic trace by a horizontal offset between the source and receiver locations for said seismic trace. A depth migration process is applied to the seismic data to obtain a first set of migrated data, and to the offset-modulated data to obtain a second set of migrated data. For each shot, offset values are estimated and associated with respective subsurface positions, by a division process applied to the first and second sets of migrated data. | 05-29-2014 |
20140172307 | TARGET-ORIENTED 4D BINNING IN COMMON REFLECTION POINT - Methods and systems for target oriented 4D binning of seismic data are presented. A target depth horizon is selected in the vicinity of where 4D changes are expected. Respectively for each data vintage, relationships between the seismic traces and reflection bins, associated with the depth surface, are established and the seismic traces are divided into common reflection angle subsets. The best matching traces from both vintages are selected for each reflection bin and output for further processing. | 06-19-2014 |
20140180593 | Joint Inversion with Unknown Lithology - Method for joint inversion of geophysical data to obtain 3-D models of geological parameters for subsurface regions of unknown lithology. Two or more data sets of independent geophysical data types are obtained, e.g. seismic and electromagnetic. Then they are jointly inverted, using structural coupling, to infer geophysical parameter volumes, e.g. acoustic velocity and resistivity. Regions of common lithology are next identified based on similar combinations of geophysical parameters. Then a joint inversion of the multiple data types is performed in which rock physics relations vary spatially in accordance with the now-known lithology, and 3-D models of geological properties such as shale content and fracture density are inferred. The computational grid for the last inversion may be defined by the lithology regions, resulting in average geological properties over such regions, which may then be perturbed to determine uncertainty in lithologic boundaries. | 06-26-2014 |
20140188392 | NORMALIZATION SEISMIC ATTRIBUTE - A method can include providing seismic data values for a subsurface region that includes a reflector; determining a gradient magnitude value based on at least a portion of the seismic data values; normalizing the gradient magnitude value using a nonlinear normalization equation that includes a gradient magnitude variable divided by a normalization variable raised to a power that depends on an adjustable parameter; and outputting the normalized gradient magnitude value. Various other apparatuses, systems, methods, etc., are also disclosed. | 07-03-2014 |
20140188393 | EFFICIENT WAVEFIELD EXTRAPOLATION IN ANISOTROPIC MEDIA - Various examples are provided for wavefield extrapolation in anisotropic media. In one example, among others, a method includes determining an effective isotropic velocity model and extrapolating an equivalent propagation of an anisotropic, poroelastic or viscoelastic wavefield. The effective isotropic velocity model can be based upon a kinematic geometrical representation of an anisotropic, poroelastic or viscoelastic wavefield. Extrapolating the equivalent propagation can use isotopic, acoustic or elastic operators based upon the determined effective isotropic velocity model. In another example, non-transitory computer readable medium stores an application that, when executed by processing circuitry, causes the processing circuitry to determine the effective isotropic velocity model and extrapolate the equivalent propagation of an anisotropic, poroelastic or viscoelastic wavefield. In another example, a system includes processing circuitry and an application configured to cause the system to determine the effective isotropic velocity model and extrapolate the equivalent propagation of an anisotropic, poroelastic or viscoelastic wavefield. | 07-03-2014 |
20140200811 | Identifying Reservoir Drainage Patterns From Microseismic Data - A method and system for identifying reservoir drainage patterns from microseismic data for illustrating flow paths towards ports. The method includes: determining moment tensor data for each of a plurality of microseismic events in the reservoir; inferring crack formation data in the reservoir in dependence on the moment tensor data; and calculating stream lines that represent predicted flow of fluids through the reservoir in dependence on the inferred crack formation data. | 07-17-2014 |
20140200812 | PROCESSING SURVEY DATA FOR DETERMINING A WAVEFIELD - Survey data corresponding to a subsurface region of interest is received. A wavefield is determined by iteratively performing the following until a specified condition is satisfied. For a current iteration, an element that includes a representation of at least one portion of the wavefield is selected based at least in part on a current residual representing an approximation error. For the current iteration, a respective data structure is computed from the selected element. The data structure is orthogonally projected onto a space spanned by a plurality of data structures including the computed data structure. The current residual is based at least in part on the orthogonal projection. | 07-17-2014 |
20140200813 | SYSTEMS AND METHODS FOR SEISMIC DATA PROCESSING USING KINEMATIC ANALYSIS OF SOURCE-RECEIVE MIGRATION ADCIGS - Systems and methods are provided for determining a starting position and direction of a ray for use in generating a velocity model based at least in part on a kinematic analysis of Angle Domain Common Image Gathers (ADCIGs) obtained by a Wave Equation Migration (WEM) process. A method includes: determining a migrated spatial dip from a stack; determining a slope of a residual move-out (RMO); remapping a migrated value into a first value; repositioning the starting position of the ray based at least in part on the migrated spatial dip from the stack, the slope of the RMO and the first value; and computing the starting direction of the ray. | 07-17-2014 |
20140200814 | DIP TOMOGRAPHY FOR ESTIMATING DEPTH VELOCITY MODELS BY INVERTING PRE-STACK DIP INFORMATION PRESENT IN MIGRATED/UN-MIGRATED PRE-/POST-STACK SEISMIC DATA - Methods and systems for dip constrained non-linear tomography in seismic data. An additional term, comprising the dip associated with the kinematic migration of locally coherent events, is introduced into the cost function. The velocity is then updated to match the expected dip of the re-migrated offset-dependent events. Volumetric dip information can be automatically selected at a greater density in shallow locations, therefor complementing the lower density of the RMO events associated with shallow locations. | 07-17-2014 |
20140214327 | FLUID MIGRATION PATHWAY DETERMINATION - A method of determining a migration pathway of a subterranean fluid through a geological volume is provided. The starting object is located within the geological volume. The starting object defines an initial fluid boundary. Data points are distributed through the geological volume. The data points are associated with values of one or more geological attributes. The method includes the steps of: defining an expression which determines a change in position of the fluid boundary at the data points over an iteration based on the values of the one or more attributes; and applying the expression at the data points for successive iterations to evolve the fluid boundary over the successive iterations. The migration pathway of the subterranean fluid through the geological volume can then be determined from the evolution of the fluid boundary. | 07-31-2014 |
20140222345 | METHODS AND SYSTEMS OF INCORPORATING PSEUDO-SURFACE PICK LOCATIONS IN SEISMIC VELOCITY MODELS - Incorporating pseudo-surface pick locations in seismic velocity models. At least some of the illustrative embodiments are methods including: refining a seismic velocity model by correlating a predicted log to a measured log; creating a pseudo-surface pick location in a modeled subsurface horizon based on the correlating; modifying at least a portion of a seismic velocity model based on the pseudo-surface pick location; recalculating the modeled subsurface horizon based on the seismic velocity model, thereby creating a modified surface; and plotting the modified surface on a display device of a computer system. | 08-07-2014 |
20140222346 | ANALYTIC ESTIMATION APPARATUS, METHODS, AND SYSTEMS - In some embodiments, apparatus and systems, as well as methods, may operate to record a plurality of acoustic waveforms corresponding to acoustic waves received at azimuthally orthogonal dipole receiver arrays surrounded by a geological formation, the waves being generated by azimuthally orthogonal transmitter arrays. Further activity may include analytically estimating a global minimum of a predefined objective function with respect to an azimuth angle at a point in an auxiliary parameter space associated with a set of auxiliary parameters, minimizing the objective function at the analytically estimated angle with respect to the auxiliary parameters, removing existing ambiguities associated with the fast and slow principal flexural wave axes, and determining at least one property of the geological formation based on the global minimum. Additional apparatus, systems, and methods are disclosed. | 08-07-2014 |
20140244177 | TIME LAPSE MARINE SEISMIC SURVEYING EMPLOYING INTERPOLATED MULTICOMPONENT STREAMER PRESSURE DATA - In a first aspect, a method for use in a time lapse, marine seismic survey includes accessing a set of acquired, multicomponent seismic data; and interpolating a set of time lapse seismic data from the acquired seismic data. In other aspects, a program storage medium is encoded with instructions that, when executed by a computing device, perform the above method and a computing apparatus programmed to perform one or more of such methods. | 08-28-2014 |
20140249755 | METHOD AND DEVICE FOR CALCULATING TIME-SHIFTS AND TIME-STRAINS IN SEISMIC DATA - A method for calculating time-strains for two seismic data sets resulting from seismic exploration of the same subsurface structure uses selected subsets of data from the two seismic data sets to calculate time-shifts for each trace. A smooth function is fitted along each trace based on the calculated time-shifts a time derivative is applied to the smooth function to obtain time-strains along each trace. | 09-04-2014 |
20140278114 | WAVEFIELD REGULARIZATION BY 3-D WAVEFIELD DECOMPOSITION FOR GEOPHYSICAL DATA - One embodiment relates to a method of wavefield regularization for geophysical data acquisition of seismic geophysical data. Measured traces, are obtained from an array of sensors. For each grid point on a processing grid, best-fitting traces of the measured traces are found. Using the best-fitting traces, spectral amplitudes of down-going and up-going wavefields are computed. The down-going and up-going wavefields are subsequently transformed to an output grid in a space-time domain. Another embodiment relates to an apparatus for wavefield regularization of geophysical data acquisition. Other embodiments, aspects and features are also disclosed. | 09-18-2014 |
20140278115 | CONTEXT BASED GEO-SEISMIC OBJECT IDENTIFICATION - A workflow is presented that facilitates defining geocontextual information as a set of rules for multiple seismic attributes. Modeling algorithms may be employed that facilitate analysis of multiple seismic attributes to find candidate regions that are most likely to satisfy the set of rules. These candidates may then be sorted based on how well they represent the geocontextual information. | 09-18-2014 |
20140278116 | FREQUENCY-SPARSE SEISMIC DATA ACQUISITION AND PROCESSING - A method includes receiving data representing measurements acquired by seismic sensors in response to energy that is produced by shots of a seismic source. The energy that is produced by the seismic source for each shot includes a plurality of discrete frequencies of discrete frequency bands that are within a frequency range of interest and are separated by at least one excluded frequency or frequency band. The data may be processed to determine at least one characteristic of a geologic structure. | 09-18-2014 |
20140288837 | ESTIMATING TRANSLATIONAL DATA - Translational data acquired by at least one seismic sensor is received. Gradient sensor data acquired by at least one gradient sensor is received. Estimated translational data at a position away from at least one position of the at least one seismic sensor is computed, where the computing is based on the gradient sensor data and the translational data. | 09-25-2014 |
20140288838 | SYSTEM AND METHOD FOR INTERPOLATING SEISMIC DATA - A system and method of interpolating seismic data is provided. The system and method form a plurality of pairwise Hankel tensors from acquired seismic data, and a respective pairwise Hankel tensor for each of a plurality of originally collected frequency slices, perform tensor completion on each of said pairwise Hankel tensors to recover a plurality of interpolated frequency slices, and combine said plurality of interpolated frequency slices with said originally collected frequency slices to form a set of trace data of a geographical area of interest. | 09-25-2014 |
20140297188 | TIME-FREQUENCY REPRESENTATIONS OF SEISMIC TRACES USING WIGNER-VILLE DISTRIBUTIONS - Presented are methods and systems for reducing or eliminating spurious error or cross-terms when using bilinear functions in a time-frequency analysis. A maximum entropy method is applied to a Wigner-Ville distribution of seismic traces to provide a robust and high resolution time-frequency representation of the seismic traces. | 10-02-2014 |
20140303896 | Method for Quantitative Definition of Direct Hydrocarbon Indicators - Method for automated and quantitative assessment of multiple direct hydrocarbon indicators (“DHI's”) extracted from seismic data. DHI's are defined in a quantitative way ( | 10-09-2014 |
20140309938 | SPHERICAL HELIX PROJECTION MICROSEISMIC NETWORK - Methods and systems for designing or configuring a microseismic monitoring network are described. The design is based on a regular and homogeneous repartitioning of seismic sensor locations associated with a focal sphere. The methods and systems determine an optimal sampling of the focal sphere of microseismic events and a takeoff angle associated with each of the optimal sampling points. The sampling points are propagated to the surface based on the associated rays and any of a plurality of ray tracing techniques. | 10-16-2014 |
20140324354 | TRANSMISSION COEFFICIENT METHOD FOR AVO SEISMIC ANALYSIS - The transmission coefficient method for AVO (amplitude variation with offset) seismic analysis computes incident-to-transmitted pressure wave and incident-to-transmitted shear wave data in a manner that is compatible with existing AVO applications for analysis on the transmission coefficients of VSP data. Amplitude variation with offset (AVO) computation techniques known in the art provide estimates of pressure wave, shear wave and pseudo-Poisson's reflectivity. Such estimates are based on the Aki-Richards approximation of Zoeppritz's formulation of reflection amplitude and polarity variation with respect to incidence angle. The Zoeppritz equations describe the amplitudes of body waves when incident on an interface, resulting in a scattering matrix in which all possible incident and generated modes are addressed. The present method further simplifies the Aki and Richards computations to facilitate further AVO analysis. | 10-30-2014 |
20140324355 | FRACTURE DETECTION USING MONOPOLE SOURCE IN ACOUSTIC WELL LOGGING - The present disclosure relates generally to well logging and measurement in subterranean formations and more particularly, the present disclosure relates to a system and method for identifying anisotropic formations, such as fractures and fracture patterns, in subterranean formations. The method uses waveforms transmitted from a monopole source. After finding the Root Mean Square energy from at least four quadrants, the energy data is normalized. At least one minimum RMS energy point is identified and the azimuth of that minimum is also identified. The azimuth and the minimum are instructive in defining fracture patterns and characteristics. | 10-30-2014 |
20140336939 | Use of Vector Rotational Measurements and Vector Pressure Gradient Measurements to Enhance Spatial Sampling of Dual-Sensor Water Bottom Seismic Data - Disclosed herein are various embodiments of a method and apparatus to enhance spatial sampling in all nominally horizontal directions for Dual-Sensor seismic data at the bottom of a body of water such as the ocean. The sensor apparatus on the water bottom is comprised of sensing elements for linear particle motion, for rotational motion, for pressure measurement, for pressure gradients, and for static orientation. Stress and wavefield conditions known at the water bottom allow numerical calculations that yield enhanced spatial sampling of pressure and nominally vertical linear particle motion, up to double the conventional (based on physical sensor locations) Nyquist spatial frequency in two nominally horizontal independent directions. The method and apparatus have a wide range of application in Ocean Bottom Seismic 3D, 4D, and Permanent Reservoir Monitoring surveys, and other marine seismic surveys, in oil and gas exploration and production. | 11-13-2014 |
20140336940 | ESTIMATION OF Q-FACTOR IN TIME DOMAIN - A method can include receiving seismic traces associated with a geologic environment; determining time domain stretch values for individual wavelets in at least a portion of the seismic traces with respect to a spatial dimension of the geologic environment; and estimating at least one Q-factor value for at least a portion of the geologic environment via a comparison of the time domain stretch values to a Q-factor model. | 11-13-2014 |
20140343859 | TIME-LAPSE 4D SCATTERING FOR IMAGING HYDRAULICALLY INDUCED FRACTURES - Tools and methods for monitoring a subterranean formation is provided. Methods for monitoring include: creating a time-lapse azimuth stack between an azimuth stack on a first seismic survey and an azimuth stack on a second seismic survey; identifying a lowest root mean square energy and a highest root mean square energy for each time-lapse azimuth stack; and recording an azimuth with largest overall root mean square energy. | 11-20-2014 |
20140350861 | MULTI-PARAMETER INVERSION THROUGH OFFSET DEPENDENT ELASTIC FWI - Method for multi-parameter inversion using elastic inversion. This method decomposes data into offset/angle groups and performs inversion on them in sequential order. This method can significantly speed up convergence of the iterative inversion process, and is therefore most advantageous when used for full waveform inversion (FWI). The present inventive approach draws upon relationships between reflection energy and reflection angle, or equivalently, offset dependence in elastic FWI. The invention uses recognition that the amplitudes of small angle (near offset) reflections are largely determined by acoustic impedance alone ( | 11-27-2014 |
20140358445 | Automated Interpretation Error Correction - A fully automated method for correcting errors in one interpretation ( | 12-04-2014 |
20140365131 | REGULARIZATION OF MULTI-COMPONENT SEISMIC DATA - Presented are methods and systems for regularizing content of multi-component seismic data. The method includes a step of receiving the seismic data, wherein the seismic data includes pressure and particle motion measurements and a step of regularizing and frequency optimizing the seismic data to desired positions based on Fresnel zones selected at various depths in a subsurface to obtain a regularized seismic dataset. | 12-11-2014 |
20140365132 | METHOD FOR DECOMPOSING COMPLEX OBJECTS INTO SIMPLER COMPONENTS - Method for decomposing a complexly shaped object in a data set, such as a geobody ( | 12-11-2014 |
20140365133 | METHODS OF AND APPARATUSES FOR IMPROVING LOG DATA - Disclosed herein is method of computing formation attributes from acoustic measurements in a borehole. The acoustic measurements can be made by operating an acoustic source at multiple frequencies to excite the formation and operating receivers at multiple, longitudinally spaced receiver stations to receive acoustic energy from the formation. The method can include: deriving phase data from the spectrum of received acoustic signals; unwrapping phase information of the phase spectrum data; determining two or more values of difference of phase between acoustic signals at each of a range of frequencies each based on a single generated signal received at two or more pairs of adjacent said receiver stations; generating a value of slope of phase difference values; and in any case of slope ambiguity, unwrapping phase difference information and deriving a dominant slope, at each frequency, from which slowness of the acoustic signal in the formation can be derived. | 12-11-2014 |
20140365134 | Method Discriminating Between Natural And Induced Seismicity - The invention pertains generally to the field of seismicity. The method of the invention provides an objective criteria for decision when determining whether or not the seismic activity (seismicity) occurring within a certain area is induced by human activity, specifically geophysical activity, particularly associated with the mining/extracting industry, or whether the seismicity is naturally occurring. The method can be useful for production companies, regulatory authorities, or insurance companies. | 12-11-2014 |
20150032378 | PREDICTING INTERBED MULTIPLES IN SEISMIC DATA USING BEAM DECOMPOSITION - A method of attenuating interbed multiples in multiply-reflected seismic waves is performed at a computer system, the method comprising: providing multiple beams of seismic data and an earth model related to a geological volume; selecting one of the beams as an input beam associated with a pair of source and detector located near a top surface of the geological volume; determining at least one of (i) a source-side stationary pegleg arrival and a corresponding detector-side primary beam and (ii) a detector-side stationary pegleg arrival and a corresponding source-side primary beam; predicting an interbed multiples beam using at least one of (i) the detector-side primary beam delayed by the source-side stationary pegleg arrival and (ii) the source-side primary beam delayed by the detector-side stationary pegleg arrival; and deconvolving the predicted interbed multiples beam with the input beam to remove at least a portion of interbed multiples present in the input beam. | 01-29-2015 |
20150032379 | ATTENUATION OF MULTIPLE REFLECTIONS - A method can include receiving an inside stack and an outside stack; generating a multiple reflections model based at least in part on the inside stack and the outside stack; receiving multidimensional seismic data that includes representations of primary reflections and multiple reflections; and generating processed multidimensional seismic data by applying the multiple reflections model to the multidimensional seismic data. Various other apparatuses, systems, methods, etc., are also disclosed. | 01-29-2015 |
20150039236 | DETERMINING AN INTERVAL BETWEEN ACTIVATIONS OF AT LEAST ONE SURVEY SOURCE - A shot interval between activations of at least one frequency-controllable survey source is determined, where the shot interval is determined based on an expected frequency of an output of the at least one frequency-controllable survey source. The at least one frequency-controllable survey source is activated using the determined first shot interval. | 02-05-2015 |
20150057936 | COMPUTERIZED METHOD OF CHARACTERIZING A GEOLOGICAL REGION OF INTEREST AND COMPUTER PROGRAM IMPLEMENTING THIS METHOD - A data set comprises data obtained by seismic imaging of a region of interest during an observation period. An intrinsic geological variability of a region is determined from the comparison of reception signals for neighbour bins as a function of a difference in signal geometry for the neighbour bins. | 02-26-2015 |
20150057937 | MICROSEISMIC EVENT LOCALIZATION USING BOTH DIRECT-PATH AND HEAD-WAVE ARRIVALS - The present invention relates to methods and apparatuses for using head waves to greatly improve microseismic event localization accuracy, particularly in the depth dimension, by analyzing them in addition to direct path arrivals whenever they are observed. Embodiments of the invention also include techniques known as multipath analysis. | 02-26-2015 |
20150073714 | VSP SYSTEMS AND METHODS REPRESENTING SURVEY DATA AS PARAMETERIZED COMPRESSION, SHEAR, AND DISPERSIVE WAVE FIELDS - Disclosed vertical seismic profiling (VSP) survey systems and method acquire multi-component signal data and represent the signal data in terms of a combination of parameterized compression, shear, and dispersive wavefields. Multiples of each wavefield type may be included, e.g., to separate upgoing and downgoing wavefield components. A nonlinear optimization is employed to concurrently estimate an incidence angle and a slowness value for each wavefield. For the dispersive wavefield(s), the slowness may be parameterized in terms of a phase slowness and a group slowness with respect to a central wave frequency. The parameter values may vary as a function of depth. | 03-12-2015 |
20150073715 | SEISMIC SURVEY ANALYSIS - A method can include receiving data sets where each of the data sets corresponds to one of a plurality of individual emitter-detector arrangements; calculating a multi-dimensional similarity metric for one of the data sets; and, based at least in part on the multi-dimensional similarity metric, assessing the one data set. | 03-12-2015 |
20150081223 | MICROSEISMIC SURVEY - Methods, computing systems, and computer-readable media for processing seismic data. The method may include obtaining a model of a subterranean domain, and determining one or more synthetic waveforms for one or more events located in the subterranean domain, based at least partially on the model. The method may also include identifying, using a processor, one or more arrival waves in the one or more synthetic waveforms, wherein at least one of the one or more arrivals represents a mode-converted wave, and generating a processing chain for determining at least a location of an event in the subterranean domain based at least partially on the at least one mode-converted wave. | 03-19-2015 |
20150088428 | COMPUTATIONALLY EFFICIENT NONLINEAR STRUCTURAL ANALYSIS - Seismic displacement demands for design of a bridge frame structure are typically determined from linear-elastic analysis (LEA), which are often incorrect, and compared to displacement capacity from a nonlinear pushover analysis. Nonlinear time-history analysis (NTHA) provides the most realistic assessment of displacement demands because it properly models the physics of the dynamic problem, wherein stiffness of the bridge varies over time. However, using NTHA to determine a bridge response from multiple earthquake motions based on the stiffness method requires excessive time. A unique approach for determining the nonlinear time-history response of a bridge frame is disclosed that is thousands of times faster than the stiffness method while providing the same results. Computational efficiency allows bridge design engineers to use NTHA for the seismic design of bridge structures by producing multiple determinations in less than one second. Displacement demands and capacities are based on nonlinear bridge behavior, resulting in safer bridge structures and reduced construction costs. | 03-26-2015 |
20150100241 | PROCESSING DATA REPRESENTING A PHYSICAL SYSTEM - A method is provided of processing data representing a physical system, the method comprising: providing (P | 04-09-2015 |
20150106019 | SYSTEM AND METHOD FOR REGULARIZING SEISMIC DATA - A system and method for regularizing irregularly sampled 5D seismic data by assigning each trace to a common midpoint bin and mapping each trace to an offset vector tile (OVT) with a calculated center azimuth; assembling an azimuth sector with all offsets of interest and a narrow range of the center azimuths from the OVTs; rotating the azimuth sector to align with an inline direction and a crossline dimension; selecting a subset of traces with a single crossline value to create an irregular 3D volume; regularizing the irregular 3D volume; and repeating as necessary to generate a regularly sampled seismic dataset. The regularization may include interpolation by an algorithm such as an anti-leakage Fourier interpolator. The regularly sampled seismic dataset may be used to characterize the subsurface by further processing such as tomography. | 04-16-2015 |
20150112600 | Spectrum Splitting - Spatial sampling is a key factor in determining acquisition parameters for seismic surveys. Acquiring the data to meet spatial sampling requirements for low, mid and high frequencies, by acquiring coarse, medium and fine acquisition grids respectively and layering these during processing, can result in reduced cost and/or higher quality surveys. | 04-23-2015 |
20150112601 | Processing Seismic Data by Nonlinear Stacking - Seismic data processing using one or more non-linear stacking enabling detection of weak signals relative to noise levels. The non-linear stacking includes a double phase, a double phase-weighted, a real phasor, a squared real phasor, a phase and an N-th root stack. Microseismic signals as recorded by one or more seismic detectors and transformed by transforming the signal to enhance detection of arrivals. The transforms enable the generation of an image, or map, representative of the likelihood that there was a source of seismic energy occurring at a given point in time at a particular point in space, which may be used, for example, in monitoring operations such as hydraulic fracturing, fluid production, water flooding, steam flooding, gas flooding, and formation compaction. | 04-23-2015 |
20150120197 | Method of Transforming Reservoir Properties to a Seismic Attribute for Hydrocarbon and Lithology Identification - Embodiments of a method for transforming petrophysical properties into seismic attributes are disclosed herein. Embodiments of the method utilize an AVO expression which maps lithology to P-wave reflectivity at a particular angle through their λ/μ values (or equivalent elastic properties K/μ and γ). Rocks with different λ/μ will be projected to the different angle and reflectivity. The equation which transforms λ/μ to reflection angle may be referred to as a Generalized Angle Transform Equation (GATE). Further details and advantages of various embodiments of the method are described in more herein. | 04-30-2015 |
20150120198 | SYSTEM AND METHOD FOR ANALYZING MICROSEISMIC EVENTS USING CLUSTERS - According to an embodiment, a method for analyzing microseismic events associated with hydraulic fracturing detects a new microseismic event and assigns it to a cluster of other events having similar characteristics. Cluster characteristic(s), e.g., average event(s), average source mechanisms, and/or average locations, are updated and used to characterize a future microseismic events. | 04-30-2015 |
20150120199 | Multiple Domain Processing For Combining Reservoir Models and Seismic Data - Method for using a non-stationary, multi-scale domain transformation to combine multiple geophysical data sources, for example seismic data and well log data, into one coherent reservoir model. The seismic data are inverted ( | 04-30-2015 |
20150134259 | Constructing A Seismic Signal Using A Predicted Energy Distribution - A technique includes processing seismic data indicative of samples of at least one measured seismic signal in a processor-based machine to determine basis functions that represent a constructed seismic signal based at least in part on a matching pursuit-based technique. The technique further includes basing the determination of the basis functions at least in part on a predicted energy distribution of the constructed seismic signal. | 05-14-2015 |
20150149093 | METHOD AND SYSTEM FOR EFFICIENT EXTRAPOLATION OF A COMBINED SOURCE-AND-RECEIVER WAVEFIELD - The current document is directed to computational systems and methods carried out by the computational systems for propagating a combined source-and-receiver wavefield from a first level to a next, second level with respect to depth, time, or another dimension. The methods and systems, to which the current document is directed, apply an efficient complex, combined-source-and-receiver-wavefield propagation operator to a complex combined-source-and-receiver wavefield in order to propagate the complex combined-source-and-receiver wavefield to the next level. Real source and receiver wavefields at the next, second level can then be extracted from the complex combined-source-and-receiver wavefield at the next level. | 05-28-2015 |
20150293244 | ESTIMATION OF A FAR FIELD SIGNATURE IN A SECOND DIRECTION FROM A FAR FIELD SIGNATURE IN A FIRST DIRECTION - The present disclosure is related to estimation of a far field signature in a second direction from a far field signature in a first direction. For a number of source elements, where the number of source elements corresponds to a seismic source, an impulse response in a first direction and a second direction can be determined. A transfer function that transforms a far field signature of the seismic source in the first direction to a far field signature of the seismic source in the second direction can be determined based on corresponding impulse responses in the first direction and the second direction. An estimated far field signature for the seismic source in the second direction can be determined based on the transfer function. | 10-15-2015 |
20150293247 | ANALYZING SEISMIC DATA - A system and methods for analyzing seismic data are provided herein. The method includes identifying, via a computing device, a representation of a seismic data set ( | 10-15-2015 |
20150301208 | SEISMIC DATA PROCESSING - Described herein are implementations of various technologies for a method for seismic data processing. The method may receive seismic data for a region of interest. The seismic data may be acquired in a seismic survey. The method may determine a seismic image based on the acquired seismic data and an earth model of the region of interest. The method may determine simulated seismic data based on the earth model. The method may determine an objective function that represents a mismatch between the acquired seismic data and the simulated seismic data. The method may determine a diffusion tensor using geological information from the seismic image. The method may update the earth model using the diffusion tensor with the objective function. | 10-22-2015 |
20150316668 | METHOD OF MODELLING A SUBTERRANEAN REGION OF THE EARTH - A method of modelling a subterranean region of the Earth at a first location comprises the steps of: providing geological data; selecting a plurality of facies; providing a distribution of rock physics probability with spatial dependencies; approximating the rock physics probability at the first location with at least one distribution per facies utilizing the spatial dependencies in the rock physics probability distribution; and performing a Bayesian inversion at the first location using the approximation of the rock physics probability distribution. The method may also employ a window comprising the first location and at least one further location. | 11-05-2015 |
20150316673 | Systems and Methods for 3D Seismic Data Depth Conversion Utilizing Artificial Neural Networks - Systems and methods for the conversion of stacked, or preferably, time migrated 3D seismic data and associated seismic attributes from a time domain to a depth domain. | 11-05-2015 |
20150323689 | Efficient Line Search Methods for Multi-Parameter Full Wavefield Inversion - Method for simultaneously inverting full-wavefield seismic data ( | 11-12-2015 |
20150323690 | SYSTEM AND METHOD FOR PROCESSING DATA - The present invention relates to a system and method that provides a user with an ability to use a secondary device to take a more detailed look at nuances within a captured seismic data set. The present invention allows the user to view a scaled image of the seismic data that is at a different scale than what is displayed on a primary device. Optionally, the secondary device is a mobile device that is wirelessly connected to the primary device. The present invention also enables the user to interpret the captured seismic data using the secondary device in real time while maintaining a macro view on the primary device. The user may annotate the scaled image regarding picked horizons and the information regarding the location of the annotations on the scaled image are then processed by the primary device and then scaled image on the secondary device is updated. | 11-12-2015 |
20150331122 | WAVEFORM-BASED SEISMIC LOCALIZATION WITH QUANTIFIED UNCERTAINTY - A method, a system, and a computer readable medium for analyzing a wavelet within a seismic signal are described herein. The method includes receiving a seismic signal from a seismic receiver, such as a geophone, and using a Bayesian probability method to determine an associated arrival time for the wavelet and determine an uncertainty for the arrival time of the wavelet. The method has application in hydraulic fracturing monitoring operations and in spatially mapping fractures. | 11-19-2015 |
20150338536 | P-WAVE AND S-WAVE SEPARATION OF SEISMIC DATA IN THE PRESENCE OF STATICS AND IRREGULAR GEOMETRY - Methods and systems for separating P-S wave field data are described. Slowness values for the PP mode and the PS mode are estimated and are, typically, unequal based on aliased and/or irregularly sampled data. A calculation, in the space-time domain, based on a matrix of equations, generates separated P-wave and S-wave data. The separated P-wave data and S-wave data are output for further imaging. | 11-26-2015 |
20150355352 | Industrial Sensor System and Method of Use - An industrial sensor system is disclosed. Said system comprising a communication module, a one or more sensors, and a power system. Said one or more sensors having a body and a logic board. Said one or more signals generated by said logic boards of said one or more sensors. Said logic board of said one or more sensors having a microcontroller capable of processing said one or more signals and a communication BUS capable of communicating with said communication module and other among said one or more sensors over a network. | 12-10-2015 |
20150355353 | DETECTING SUBSURFACE STRUCTURES - Systems and methods for analyzing geophysical data to identify structures in a subsurface are provided herein. In an exemplary method, an iterative optimization is performed that includes computing similarities between potential shapes and shape cluster models, updating cluster memberships and the shape cluster models, and determining if a criterion is improved from a previous iteration. | 12-10-2015 |
20150355356 | Method for Temporal Dispersion Correction for Seismic Simulation, RTM and FWI - Method for correcting seismic simulations, RTM, and FWI for temporal dispersion due to temporal finite difference methods in which time derivatives are approximated to a specified order of approximation. Computer-simulated seismic data ( | 12-10-2015 |
20150362608 | COMBINED INTERPOLATION AND PRIMARY ESTIMATION - A method for combined interpolation and primary estimation can include performing a plurality of interpolations on received seismic data, performing a plurality of primary estimations on the received seismic data, and performing a combination of interpolation and primary estimation. Performing the combination can include generating reestimated primaries via a second primary estimation with input of a second interpolation, where output of the first primary estimation is input to the second interpolation. | 12-17-2015 |
20150362623 | JOINT INVERSION OF ATTRIBUTES - A method can include receiving data associated with a multilithology geologic environment; and, based on at least a portion of the data, determining values for multiphase model parameters defined in a model space. | 12-17-2015 |
20150369627 | Heading Sensor for Deflector Angle of Attack Estimation - Embodiments relate to coupling a heading sensor to a deflector surface reference for obtaining the deflector heading which can be used in estimation of the deflector angle of attack. A method may comprise: towing a plurality of streamers behind a survey vessel in a body of water, wherein at least one deflector provides a lateral component of force to the streamers; determining a deflector heading over ground using at least measurements from a heading sensor on a surface reference corresponding to the deflector; determining a deflector velocity over ground using at least measurements from a position sensor on the surface reference; determining a water current of the body of water; and estimating a deflector angle of attack based on inputs comprising the deflector heading, the deflector velocity over ground, and the water current. | 12-24-2015 |
20150369935 | Instantaneous Isochron Attribute-based Geobody Identification for Reservoir Modeling - Automated systems and methods that provide robust identification of regions of interest for reservoir modeling are disclosed herein. One embodiment includes: obtaining a seismic image of a subsurface region; performing full-volume horizon picking and deriving an instantaneous isochron attribute (IIA) value for each point in the seismic image; identifying one or more geobodies within the seismic image based at least in part on the IIA values; and representing the one or more geobodies in a geocellular model. The identifying of geobodies may include: applying IIA value filtering to isolate intervals of rapid or slow deposition in the seismic image; determining a reservoir-non-reservoir indicator attribute value for each point in the seismic image; applying reservoir-non-reservoir indicator value filtering to isolate subintervals of presumed reservoirs or non-reservoirs in said isolated intervals; determining a pay indicator attribute value for each point in the seismic image; and applying pay indicator value filtering to isolate presumed pay zones in said isolated subintervals. | 12-24-2015 |
20150369936 | ESTIMATION OF WATER PROPERTIES FROM SEISMIC DATA - A method for estimation of water properties from seismic data can include determining a number of travel times for at least one event based, at least in part, on predefined values for a plurality of water properties, determining an alignment of data values for each of the number of travel times determined for the at least one event, and determining an estimation of a plurality of undetermined water property values based, at least in part, on the alignment of the data values for each of the number of travel times producing a high quantitative measure of a coherence value. | 12-24-2015 |
20150369938 | SYSTEM AND METHOD FOR PROCESSING SEISMIC DATA - A computer-implemented method for processing seismic data includes the determining, from the seismic data, a first amplitude attribute map at a first image depth corresponding to a shallow attenuating body, and a second amplitude attribute map at a second image or target depth. The first and second amplitude attribute maps are then normalized, and a ratio map is determined based on a ratio of the normalized first and second amplitude attribute maps. The ratio map is scaled to yield a scale factor map, which is then applied to the seismic data to compensate for effects of shallow overburden attenuation. The corrected seismic data may be used for subsurface characterization. | 12-24-2015 |
20150378039 | SYSTEM AND METHOD FOR SEISMIC IMAGING OF A COMPLEX SUBSURFACE - Seismic data may be processed to improve a geologic model of a subsurface volume of interest by receiving an initial geologic model, generating a γ-parameter family of models by perturbing parameters of an initial geologic model, migrating the seismic data using each of the models in the γ-parameter family of models to generate a set of migration images, constructing a γ-volume by scanning the set of migration images wherein each location in the γ-volume is assigned a value representing a preference of one of the migration images; and inverting the γ-volume. | 12-31-2015 |
20160003955 | METHOD TO DETERMINE OPTIMAL SPACING BETWEEN SEISMIC ENERGY SOURCES UTILIZING MUTUAL ADMITTANCE - A method for detemining an optimum spacing of seismic energy sources based on mutual admittance includes deploying a plurality of seismic energy sources along a source line, separated by a selected spacing. Seismic receivers are deployed along a receiver line orthogonal to the source line. Seismic energy is simultaneously transmitted from each of the plurality of seismic energy sources while recording signals from the seismic receivers. The transmitting and recording of signals is repeated for a plurality of different spacings between the energy sources. Seismic energy in the recorded signals is determined in separate time windows selected to represent reflected body wave signal, and source generated ground roll noise, respectively. A signal-to-noise ratio with respect to the spacing of the seismic energy sources is calculated and the optimum spacing between energy sources is selected based on the signal-to-noise ratio. | 01-07-2016 |
20160018541 | SYSTEM AND METHOD FOR ROCK PROPERTY ESTIMATION OF SUBSURFACE GEOLOGIC VOLUMES - A system and model for estimating rock properties may include receiving an initial reservoir model of the subsurface, calculating p-dependent reflection coefficients and vertical travel times at each boundary in the initial reservoir model, performing a Discrete Fourier Transform using the reflection coefficients and travel times to get a temporal spectrum of the reflectivity trace, multiplying by the temporal spectrum of a desired wavelet, performing an inverse DFT, and extracting the amplitude values at the vertical travel times for each boundary to generate synthetic seismic data. This synthetic seismic data may be compared with recorded seismic data to update the reservoir model. | 01-21-2016 |
20160018550 | DIRECT FLUID INDICATORS IN MULTIPLE SEGMENT PROSPECTS - Methods, systems, and computer-readable media for determining a chance of success for a prospect including two or more segments. The method may include receiving seismic data indicative of a plurality of anomalies in a prospect. The prospect may include a plurality of segments. Prior probabilities of success and failure scenarios may be computed for at least one of the segments of the prospect. Likelihoods of the anomalies may be determined given the success and failure scenarios for the at least one of the segments. At least two of the segments may be classified into a direct fluid indicator dependency group. A degree of correlation may be determined between the anomalies for the direct fluid indicator dependency group. A posterior chance of success may be determined for the prospect based at least in part on the degree of correlation between the anomalies. | 01-21-2016 |
20160025880 | TARGET-ORIENTED PROCESS FOR ESTIMATING FRACTURE ATTRIBUTES FROM SEISMIC DATA - Method for characterizing a subterranean formation includes: obtaining azimuth-dependent observed travel-times from measured seismic data; inverting observed travel-times to calculate a fracture attribute selected from the group consisting of: magnitude and orientation; identifying presence of fracture based on calculated fracture magnitude; identifying fracture direction based on calculated fracture orientation; calculating predicted travel-times; calculating differences or residual errors between observed travel-times and predicted travel-times; identifying potential fault locations based on residual errors; inverting fracture magnitude and orientation using travel-time differences between a shallower horizon to a deeper horizon of interest to minimize overburden artifacts. | 01-28-2016 |
20160047922 | METHODS AND SYSTEMS TO OPERATE MARINE SOURCES TO AVOID AIR IN WATER EFFECTS - In order to avoid complicated and unpredictable effects on the wavefields emitted by air guns activated at different times, methods and systems of the current disclosure are directed to computationally designing a sequence for activating subsets of air guns in a time distributed manner that minimizes the effects of air in the water surrounding the source. The sequence may be used with discrete and continuously recorded marine surveys. | 02-18-2016 |
20160047928 | METHODS AND SYSTEMS OF WAVEFIELD SEPARATION APPLIED TO NEAR-CONTINUOUSLY RECORDED WAVEFIELDS - Wavefield separation methods and systems that adjust near-continuous pressure and particle motion wavefields based on distance moved along a vessel track by the sensors when the wavefields were measured are disclosed. Methods and systems correct for the motion of the receivers in towed streamer seismic data in order to obtain a wavefield with approximately stationary-receiver locations. Wavefield separation may then be applied to the wavefield with approximately stationary-receiver locations. | 02-18-2016 |
20160054463 | CLOSED-LOOP MULTI-DIMENSIONAL INTERPOLATION USING A MODEL-CONSTRAINED MINIMUM WEIGHTED NORM INTERPOLATION - Interpolation of seismic data of a subterranean formation includes: obtaining input seismic data; constructing an initial model by interpolation operation along dominant dips in time domain, wherein the initial model includes structural features of the subterranean formation; interpolating seismic data missing from the input seismic data via model-constrained minimum weighted norm interpolation (MWNI) to generate interpolated data; computing difference between the input seismic data and the interpolated data, wherein the difference is residual data; replacing the initial model using difference between the initial model and the interpolated data to generate an updated-initial model; performing model-constrained MWNI method using the residual data and the updated-initial model; adding the interpolated data from residual data to a previously generated interpolated data. | 02-25-2016 |
20160061978 | SYSTEM AND METHOD FOR ATTENUATING MULTIPLE ENERGY IN SEISMIC DATA - A method for processing seismic data contaminated by peg-leg multiple energy may include identifying at least one peg-leg event in the seismic dataset; flattening the seismic dataset on the peg-leg event; transposing the seismic dataset so that an axis representative of the geographic space becomes the first axis; filtering the transposed seismic dataset with a low-cut filter along the first axis; and transposing the filtered seismic dataset back to its original orientation. The method may be carried out on a computer system including a processor configured to execute modules implementing the method. | 03-03-2016 |
20160070023 | A PENALTY METHOD FOR PDE-CONSTRAINED OPTIMIZATION - The invention is directed to a computer-implemented method for obtaining a physical model having physical model parameters wherein solutions to one or more partial-differential-equations (PDE's) are calculated and wherein (i) an appropriate initial model is selected, (ii) setup a system of equations referred to as the data-augmented PDE for the field, comprising of the discretized PDE, the sampling operator, the source function and the observed data, and solve the data-augmented PDE in a suitable manner to obtain a field that both satisfies the PDE and fits the data to some degree, (iii) setup a system of equations by using the PDE, the source function and the field obtained in step (ii) and solve this system of equations in a suitable manner to obtain an update of the physical model parameters and repeat steps (ii)-(iii) until a predetermined stopping criterion is met. | 03-10-2016 |
20160109589 | VELOCITY TOMOGRAPHY USING PROPERTY SCANS - Method for building a subsurface model of velocity or other elastic property from seismic reflection data using tomography. The method uses velocity scans to pick a focusing velocity model at each image point ( | 04-21-2016 |
20160109590 | METHOD AND SYSTEM OF CALCULATING HYPOCENTERS OF MICROSEISMIC EVENTS - Calculating hypocenters of microseismic events. At least some of the example embodiments are methods including: detecting seismic waves from a microseismic event, the detecting by a sensor array disposed on a seafloor, the microseismic event originating in a formation below the sensor array, and the detecting creates received data; separating the received data into up-going data and down-going data, the down-going data indicative of detected seismic waves after a first reflection of the seismic waves at a sea surface; and calculating a hypocenter of the microseismic event using both the up-going data and the first down-going data. | 04-21-2016 |
20160116618 | METHOD FOR DETERMINING A STACKED MODEL DESCRIBING ARCHITECTURAL ELEMENTS - The present invention relates to a method for determining a stacked model describing architectural elements from a plurality of architectural element. The method comprises selecting an architectural element, determining merged zone, the merged zone being function of the zone of the selected architectural element and zones of related architectural elements, determining a probabilistic zone, the probabilistic zone being a function of the merged zone, and determining a probabilistic superposition value associated with the determined probabilistic zone, the probabilistic superposition value being a function of the superposition value of the selected architectural element. The previous steps are repeated for each architectural element in the plurality of architectural elements. The method further comprises stacking every determined probabilistic zone in a stacked model according to the determined probabilistic superposition value associated therewith, and providing the stacked model. | 04-28-2016 |
20160124099 | METHOD AND SYSTEM FOR IDENTIFICATION OF GEOLOGY LITHOLOGICAL DIFFERENCE - The present invention relates to a method for identification of geology lithological difference which includes: obtaining seismic amplitude data of a geology object to be detected; using a seismic amplitude value of each grid point as the initial value of chaos nonlinear iteration equation and then to iterate by the equation, and recording an iteration convergence rate of each grid point when the iteration reaches a stable state; and depicting the lithological difference of the geology object to be detected by the difference of the convergence rate of each grid point. The solution of the present invention can identify the geology lithological difference more sensitively. | 05-05-2016 |
20160124100 | Systems and Methods for Non-Parametric Autopicking of Seismic Wave Features from Seismic Data - Systems and methods for automatically detecting and identifying seismic wave features in seismic data are provided. In general, the systems and methods utilize a nonparametric time series classification method to detect seismic wave features that may otherwise be difficult to automatically identify in seismic data. Instead of building a model by estimating parameters from the seismic data, the data itself is used to define a trained model. The systems and methods described here provide the ability to detect and identify seismic wave features with reasonably fast and extremely accurate results without needing to compute parameters. | 05-05-2016 |
20160131779 | System, Machine, and Computer-Readable Storage Medium for Forming an Enhanced Seismic Trace Using a Virtual Seismic Array - Embodiments of a system are provided for forming enhanced seismic array traces using virtual seismic sensors in addition to the real seismic sensors to form a virtual seismic array. The system receives the signal responses from the real sensors, processes the signal responses from the sensors to define virtual signals using a narrowband decomposition of the complex envelope of the sensor signal responses, calculates second- and fourth-order statistics to derive steering vectors for the array of real sensors, and forms a virtual seismic array in response thereto. Machines, computer program product, and computer-implemented methods are provided for forming enhanced seismic array traces by receiving the array responses from sensors, processing the signals to define virtual sensor signals and a virtual seismic array, and forming an array response for the virtual seismic array to form a seismic trace of enhanced resolution. | 05-12-2016 |
20160146958 | Method and Computer System for Determining Seismic Node Position - A computing system and method for determining the x, y energy receiver (node) positions regardless of the angle at which the energy was released from the source. The process and computing system involves an iterative looping technique that is executed in data processing software wherein an initial model position based on, in essence, a best guess as to a node's location, followed with the iterative process of statistically comparing model data to actual data and then adjusting the model position by some predetermined amount and comparing this new result to the actual data to determine if the newly adjusted position is statistically better or worse than the originally selected position assumption. The process can be repeated using continuously smaller distance adjustments to the previously determined best position. Once satisfied that the true best position has been achieved, the processing can cease and the XY position data may be used in the normal course of generating seismic maps. | 05-26-2016 |
20160154130 | MODEL-BASED TIME-PRESERVING TOMOGRAPHY | 06-02-2016 |
20160187506 | METHOD FOR ITERATIVE INVERSION OF DATA FROM COMPOSITE SOURCES - Iterative inversion of composite source data obtains recorded seismic data at a plurality of receivers from a plurality of sources. A selected orthogonal function is applied to a set of sources selected from the plurality of sources to identify candidate sources in the set of sources to receive a time shift. A time shift is applied only to the candidate sources, and all sources in the set of sources are combined into a composite source. A current earth model performs forward modeling for the composite source to generate a synthetic seismic data set. A composite recorded seismic data set associated with the set of sources at the receivers is determined and is used with the synthetic seismic data set to determine a residual seismic data set. The current earth model performs a gradient update that is used to update the current earth model and generate an updated earth model. | 06-30-2016 |
20160202370 | SYSTEM AND METHOD FOR GENERATING A DEPOSITIONAL SEQUENCE VOLUME FROM SEISMIC DATA | 07-14-2016 |
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20170235001 | METHOD AND APPARATUS FOR MEASURING SEISMIC DATA | 08-17-2017 |
20190146108 | SYSTEM AND METHOD FOR ASSESSING THE PRESENCE OF HYDROCARBONS IN A SUBTERRANEAN RESERVOIR BASED ON SEISMIC DATA | 05-16-2019 |