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Elastic Full-Waveform Inversion Using Migration-Based Depth Reflector Representation in the Data Domain
The depth velocity model is a critical element for providing seismic data processing success, as it is responsible for the times of waves' propagation and, therefore, prescribes the location of geological objects in the resulting seismic images. Constructing a deep velocity model is the most time-consuming part of the entire seismic data processing, which usually requires interactive human intervention. This article introduces the consistently numerical method for reconstructing a depthdoi:10.3390/geosciences11020076 fatcat:ttw3uitfdjbczlc3zr376tiouq