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New Technology

ES360

Full azimuthal migration. Is applied for calculating the wave field in anisotropic environment and calculation of porosity attributes

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RTM

Reverse Time Migration. Is applied in difficult geological conditions complicated by salt tectonics

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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

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FWI

FWI algorithm is based on modeling synthetic gathers using initial velocity model and minimization of difference between real and modeled gathers

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5D-Regularization

5D-Regularization and Pre-Stack Time Migration

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