Integrated Stratigraphic And Structural Interpretation Of The Fluvio-Marine To Deltaic Depositional Environment In Jambu Field, Malay Basin

Jambu Field consist of a major fault series which having strike trends of N-S and one major fold-and-thrust belt structure striking E-W which mainly derived from major tectonic activity by N-S compressional stress of the Malay Basin during Miocene. Major faults is identified throughout Group H of Jambu Field, Malay Basin together with evidence of channel presence.