Publications

Sea level drops in the South Palembang Sub Basin during Late Early Miocene were obviously identified. The seismics, well logs, and paleontological data indicate the occurence of sea level drops in late N-6 that formed the N-6 sequence boundary. In late N-7 another drop caused the N-7 sequence boundary. The effects of the sea level drop occured during the Late N-6 were identified in Lower Talang Akar Formation. The sea level drop of N-6 formed thick sand bodies which could be as reservoirs, and the late N-7 sea level drop produced the secondary porosity for hydrocarbon carbonate reservoirs in this area.