New Technology
ES360
Full azimuthal migration. Is applied for calculating the wave field in anisotropic environment and calculation of porosity attributes
RTM
Reverse Time Migration. Is applied in difficult geological conditions complicated by salt tectonics
QPSDM
The use of Q migration allows you to restore high frequencies, as a result of their absorption by the medium, due to which the resolution increases seismic recording
FWI
FWI algorithm is based on modeling synthetic gathers using initial velocity model and minimization of difference between real and modeled gathers
