“…The imaging of subsurface structures to obtain information on stratigraphic features and structures in geological fields requires the determination of the field of propagation velocities of the seismic waves at each subsurface position. Obtaining this velocity field has been constantly researched in the applied geophysical and represents a crucial part of techniques, such as: seismic tomography (BOZDA G; TRAMPERT; TROMP, 2011;CERQUEIRA;CUNHA, 2016;RAWLINSON et al, 2014), seismic migration (MENKE, 2012), full waveform inversion (DATTA; SEN, 2016;JIN;CAO;YIN, 2020;SAJEVA et al, 2016), ray tracing (HANYGA; SEREDY ŃSKA, 2020), and among others (ELY; MALCOLM; POLIANNIKOV, 2018; MOLLEHUARA-CANALES et al, 2021;STUART;MINKOFF;PEREIRA, 2019).…”