Global Footprint

Foreland Basin

Direct 3D structural mapping of structures with weak seismic response

Thrust/Fold Belt

Defining the Pelarang Anticline an area of difficulty for traditional seismic methods

Basement lithologies of variable composition surrounded by basins on its northwest, north, east and south margins.

Direct 3D mapping of basement structures

Nordkapp Basin - Late Paleozoic sedimentary basin with a high level of salt diapirism

Enhance understanding of salt body geometry

Mapping Carbonate build up structures

Carbonate build up strutures

Assessing Carbonate Build-Ups and their likely composition

Directly mapping - Top Basement, Principal Fault trends, Syn-Rift plays, Anticlinal closures, Potential for Shale Diapirism, Carbonate Build-Ups

Directly mapping - Top Basement, Principal Fault trends, Syn-Rift plays, Anticlinal closures, Potential for Shale Diapirism, Carbonate Build-Ups

Directly mapping - Top Basement, Principal Fault trends, Syn-Rift plays, Anticlinal closures, Potential for Shale Diapirism, Carbonate Build-Ups

Large scale sedimentary basin

Mapping the shallow section with high resolution FTG assist drill hazard analysis and shallow velocity modelling

2011 discovery and regional gravity data proves that the Mannar Basin contains basaltic traps, sub basins as well as possible gas leakage from fractures. Thus, it is important to map the traps and identify these fractures to find source rock(s). As the geology of the study area is of Rift type, FTG is used to speed up the exploration which saves time, cost and delineate sub-basins and structures clearly, defining better targets.

67,000 sq kms of re-processed FTG data, useful for imaging salt structure in hydrocarbon exploration