Paper Summary
Integration of 3D seismic reflectivity data and well logs in AVO studies have led the way in the characterization of the Paleocene deposits in the mature South Viking Graben. However, there are limitations in these techniques, in some instances highly anisotropic facies, such as volcanic tuffs, might show a similar response to well-known reservoir sands. To overcome this issue, we present an innovative workflow that integrates isotropic information derived from the recently acquired multi azimuth multisensor survey into AVO workflows. Results are promising, as the seismic isotropic information increases our ability discriminating volcanics from clastics, revealing the internal geometry of the deep-water fan system, and opportunities in this mature area