A A series of tectonic events from time to time (tectonic evolution) that everoccured in Musi Rawas Area and surroundings, showing the existence of twomajor force phases. There are Paleogene Extensional and Plio-PleistoceneCompressional. Those two major phases resulted the subsurface physiography of Musi Rawas Area into Higher and Deeper blocks. As the results of PaleogeneExtensional major force phase, there are Paleo Musi High located in the centerand widen to the southern of observation area, Benakat Gulley to the east, andKlingi Deep/Pigi Trough to the west. And the results of Plio-Pleistocenecompressional major force phase, showed by newer blocks with northwestsoutheast general trend that folded, lifted and even inverted/thrusted. Those subsurface physiography which resulted by series of tectonic events, provided six exploration play types in this area; (1) Thrust/Inversion Related Structure; (2) Sub-Thrust/Inversion Related Structure; (3) Basement Fracture; (4) Main Anticlinal Trend; (5) Stratigraphic Trap (Associated with seismic unconformity); and (6) Build Up Reef. Petrophysical analysis of Andar-1 log data provided three reservoir intervals; (1) 1601m - 1607m (net pay = 6m, ϕe = 0.1752, Sw = 0.445); (2) 1691.2m - 1696.2m (net pay = 3.4m, ϕe = 0.1872, Sw = 0.457); and (3) 2150.5m – 2156m (net pay = 4.6m, ϕe = 0.1515, Sw = 0.437). In this Area, there are three prospects which considered as the best prospects that observer has evaluated. Two of the prospects are related to Thrust/Inversion Structure play type, and the rest of them is related to Main Anticlinal Trend play type. Those chosen prospects are proceeded to hidrocarbon in place calculation, with total Recoverable Resources (P50); Prospect 1 = 81.5 BSCF, Prospect 2 = 60.8 BSCF, Prospect 3 = 22.6 BSCF