A method for use in seismic exploration comprises: accessing a set of seismic data representative of a subterranean geological formation and a subsurface attribute model of the subterranean geological formation; performing a wavefield extrapolation on the seismic data in the subsurface attribute model; applying the time-shift extended imaging condition to the extrapolated wavefields; forming shot-indexed, time shift gathers for each image pixel of the subsurface attribute model from the conditioned extrapolated wavefields; adaptively focusing the gathers; and stacking the adaptively focused gathers; and imaging the subterranean geological formation from the stacked, adaptively focused gathers. The method may, in some aspects, be realized by a computing apparatus programmed to perform the method or as a set of instructions encoded on a non-transitory program storage medium that, when executed by a computing apparatus, perform the method.

A sonic logging method is provided that transmits acoustic signals using a high order acoustic source and processes waveform data to identify a set of arrival events and time picks by automatic and/or manual methods. Ray tracing inversion is carried out for each arrival event over a number of possible raypath types that include at least one polarized shear raypath type to determine two-dimensional reflector positions and predicted inclination angles of the arrival event for the possible raypath types. One or more three-dimensional slowness-time coherence representations are generated for the arrival event and raypath type(s) and evaluated to determine azimuth, orientation and raypath type of a corresponding reflector. The method outputs a three-dimensional position and orientation for at least one reflector. The information derived from the method can be conveyed in various displays and plots and structured formats for reservoir understanding and also output for use in reservoir analysis and other applications.

Modeling basin geology in a subsurface region includes receiving seismic data representing acoustic signals that are reflected from regions of the subsurface; receiving potential fields data comprising potential field values that are mapped to locations in the subsurface; determining a relationship between the seismic data and the potential field values for each of the locations in the subsurface; generating, based on the relationship for each location, a three-dimensional (3D) map of thermal conductivity in the subsurface region; and based on the 3D map of thermal conductivity, identifying at least one area comprising source rock having a threshold maturity, the threshold maturity indicative of potential hydrocarbons in the subsurface.

A method can include receiving seismic survey data of a subsurface environment from a seismic survey utilizing water bed receivers, where each of the receivers includes a clock; assessing one or more clock calibration criteria; based on the assessing, selecting a clock drift processor for processing at least a portion of the seismic survey data from a plurality of different clock drift processors; using at least the clock drift processor, performing a simultaneous inversion for values of model-based parameters; and, using at least a portion of the values, generating processed seismic survey data that represents one or more geological interfaces in the subsurface environment.

Embodiments herein relate to a computer-implemented technique that includes generating, in a first portion of a graphical user interface (GUI), a first graphical element related to reflection seismic data of an area of interest. The technique further includes generating, in a second portion of the GUI, a second graphical element related to well structural data of the area of interest. The technique further includes generating, in a third portion of the GUI, a third graphical element that is based on the reflection seismic data and the well structural data. In embodiments, an alteration of the first graphical element or the second graphical element results in a concurrent alteration of the third graphical element. Other embodiments may be described or claimed.

An optical seismic surveying system including, a multibeam laser source including a plurality of laser-sources, a Diffractive-Optical-Element (DOE), an imager and a processor. The laser-sources direct respective laser-beams toward a single common focal point. The DOE is located at a single common focal point and configured to split each laser-beam into a plurality of laser-beams, toward an instantaneous area of interest. The laser-beams impinging on the instantaneous area of interest produce a laser spot assemblage including a plurality of laser spots. The imager acquires a plurality of defocused images of speckle patterns produced by diffused reflections of the laser spots. The speckle pattern correspond to a respective laser spot and thus to a respective sensing point in the instantaneous area of interest. The processor determines a relative displacement between corresponding speckle patterns in sequential pairs of images and determines a respective time-signal for each sensing point representing vibrations thereat.

The disclosure relates to determining rock properties of subterranean formations and learning the distribution of hydrocarbons in the formations. A geometrical element spread function is disclosed that quantifies distortion of the geology as seen by the geophysicists who process seismic images of the subterranean formations. A method of determining the rock properties using the seismic images and synthetic images is provided. In one example, the method includes: (1) obtaining seismic data from a subterranean formation using a seismic acquisition system, (2) generating one or more seismic images of the subterranean formation using the seismic data, (3) creating one or more synthetic images from the one or more seismic images, and (4) determining rock properties of the subterranean formation based on the one or more seismic images and the one or more synthetic images.

A drilling tool for determining a real-time image of a borehole during drilling of the borehole, comprising: a drillstring, an acoustic caliper attached to the drillstring including: an acoustic transmitter that transmits a transmitted acoustic pulse, and an acoustic receiver that receives a reflected acoustic pulse, a well positioning device that determines a depth and accurate position of the acoustic caliper in the borehole, and a Programmable Logic Controller (PLC) that determines, in real-time, the time of flight of the acoustic pulse between transmitting the transmitted acoustic pulse and receiving the reflected acoustic pulse of the acoustic caliper, determines, in real-time, a distance between the acoustic caliper and a borehole wall based on the time of flight, and determines, in real-time, an image of the borehole wall during drilling of the borehole based on the distance as function of the depth and accurate position.

A method and system for forming a depth-domain seismic image using a predicted seismic velocity model is disclosed. The method includes obtaining a first surface seismic dataset of a subterranean region and obtaining a measured seismic velocity profile through the subterranean region for a surface location. The method also includes determining a set of seismic attributes for the surface location from the first surface seismic dataset, and training, using the measured seismic velocity profile and the set of seismic attributes, a machine-learning network to predict a predicted seismic velocity profile from the set of seismic attributes, wherein the predicted seismic velocity profile is an estimate of the measured seismic velocity profile. The method further includes determining a set of seismic attribute volumes from a second surface seismic dataset, and predicting a seismic velocity model for the subterranean region, using a trained machine-learning network and the set of seismic attribute volumes.

A method for determining an internal multiple attenuated seismic image is disclosed. The method includes obtaining a seismic dataset composed of a plurality of seismic traces and for each seismic trace determining an internal multiple trace based, at least in part, on a nested truncated correlation and a bounded convolution of the seismic trace with itself. The method further includes determining an internal multiple attenuated seismic trace based, at least in part, on subtracting the internal multiple trace from the seismic trace and combining the internal multiple attenuated seismic trace to form the internal multiple attenuated seismic image. A system including a seismic source, a plurality of seismic receivers, and a seismic processor for executing the method is disclosed.