China Petroleum Exploration ›› 2016, Vol. 21 ›› Issue (2): 69-77.

• PETROLEUM GEOLOGY • Previous Articles     Next Articles

Main factors controlling accumulation of overpressured gas reservoir in Block D, Myanmar

Shi Lei1,Li Fuheng2,Yin Jinyin1,Tian Naxin1,Guo Jinrui1,Zhu Weihua3   

  1. 1 Petroleum Exploration and Development Research Institute of SINOPEC
    2 PetroChina Research Institute of Petroleum Exploration and Development
    3 Research Institute of Exploration and Development SINOPEC Jianghan Oilfield Company
  • Online:2016-03-16 Published:2016-03-16

Abstract: Block D in Myanmar is located along the hydrocarbon-richest west deep depression zone in the Ayeyarwady Basin. Presently, high-yield gas flows have been obtained through testing of 3 wells drilled in Taben Formation of Eocene System, indicating that this block has a certain exploration potential. However, this block features a low overall degree of exploration, widespread presence of overpressure in major target layers of Eocene, complicated accumulation conditions and unclear main factors controlling enrichment of hydrocarbon within overpressure system, thus significantly increasing future exploration risks. Through statistical analysis of worldwide representative overpressure hydrocarbon reservoirs and correlated analysis carried out in adjacent counterparts according to the latest geologic knowledge and exploration results regarding Block D, it is believed that two sets of source rocks exist in Block D – Taben and Langshing. The autochthonously developed source rocks of Taben Formation are characterized by shallow buried depth and low degree of evolution. Accordingly, the hydrocarbon is supposed coming from genetic depressions adjacent to the block or the source rock of Langshing Formation deep down. Accumulation inside the overpressure zone in Block D is primarily controlled by reservoir and preservation conditions. The effective migration-transport system and spatiotemporal allocation are important factors for hydrocarbon enrichment. Block D is lack of high-quality reservoirs of Oligocene like in the south Salin depression and its major reservoirs feature medium-porosity, low-permeability sandstone of Taben Formation; therefore, high importance should be attached to secondary pore and fracture intervals in the overpressure system vertically. The lower wall of the fault in Block D is an important area of exploration due to its relatively good hydrocarbon preservation conditions.

Key words: Block D in Myanmar, accumulation conditions, overpressure, main factors controlling accumulation, area of exploration