Abstract:
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.
Abstract:
Disclosed herein is a system and method for building a velocity model for a geographical area of interest (GAI). The system and method comprise determining a ray based tomography velocity image of said GAI using acquired data, determining a high resolution velocity guide (HRVG) image of said GAI, scaling said determined HRVG of said GAI, adding the scaled HRVG to the ray based tomography velocity image to determine an updated ray based tomography velocity image, and determining whether said updated ray based tomography velocity image has experienced convergence by determining whether a cost function of said ray based tomography velocity image does not improve compared to a previously determined cost function value of said ray based tomography velocity image.
Abstract:
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.
Abstract:
A preserved-amplitude RTM-based FWI method is used to obtain an image of an explored subsurface formation. Model data corresponding to detected data is generated using a velocity model of the formation. Residuals representing differences between the modeled data and the detected data are back-propagated to then update the velocity model a local optimization based on a deconvolution formula employing a backward propagating wavefield and a forward propagating wavefield. Geophysical features of the formation are imaged based on the updated velocity model.