New Technology
ES360
Full azimuthal migration. Is applied for calculating the wave field in anisotropic environment and calculation of porosity attributes
![SeismicImages](images/Seis1.jpg)
RTM
Reverse Time Migration. Is applied in difficult geological conditions complicated by salt tectonics
![SeismicImages](images/Seis2.jpg)
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
![SeismicImages](images/Seis3.jpg)
FWI
FWI algorithm is based on modeling synthetic gathers using initial velocity model and minimization of difference between real and modeled gathers
![SeismicImages](images/Seis4.jpg)
![SeismicImages](images/Seis5.jpg)