principal basics
Scattered waves, re-emitted by geomedium fractures, are always present in a registering seismic wave field. Energetically they are 10-100 times weaker than a reflected component. Separating and picking these weak scattered waves up with subsequent identification and location of their origination points within the geomedium have always been the main methodical problem. Nowadays, this problem is solved by SVSL-technique for oil and gas field observation and data processing.
![[ 1 ]](companyprofilep01.gif)
![[ 2 ]](companyprofilep02.gif)
![[ 3 ]](companyprofilep03.gif)
![[ 4 ]](companyprofilep04.gif)
![[ 5 ]](companyprofilep05.gif)
![[ 6 ]](companyprofilep06.gif)
![[ 7 ]](companyprofilep07.gif)
![[ 8 ]](companyprofilep08.gif)
![[ 9 ]](companyprofilep09.gif)