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《Natural Gas Industry》 2008-01
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RELATIONSHIP BETWEEN GAS RESERVOIRS OF REEF-BANK TYPE AND TECTONIC SYSTEMS IN THE YANSHAN AND HIMALAYAN EPOCH

LI Yong-ping1,XIONG Liang2,HE Li2,LIU Li-ping2(1 Southwest Branch of SINOPEC Petroleum Engineering Company;2 Exploration and Development Research Institute of SINOPEC Southwest Branch)  
After significant breakthroughs were made in exploration of the Upper Permian Changxing Formation organic reef-bank gas reservoirs and the Lower Triassic Feixianguan Formation oolitic organic bank gas reservoirs in Puguang and Maoba areas in the northeastern Sichuan Basin,many researchers believed based on study of sedimentary facies that these reef-banks are mounded deposits distributed along Guangwang ocean trough,Chengkou-Exi ocean trough and Liangping-Kaijiang ocean trough slope break zone,where the enrichment of hydrocarbons are related with the ocean troughs.However,analysis of the superimposed structures overlying the Yanshan and Himalayan structures shows that various shear structural systems especially their relatively stable parts have influenced these reef-bank gas reservoirs in the process of hydrocarbon migrations.Based on this concept,it is predicted that large discoveries of reef-bank oil and gas reservoirs are expected in the superimposition area between relatively stable parts of Zhongtaishan and Mianyang shear structural systems and the mounded deposits on the seismic section of the underlying strata in Bazhong and Yilong lotus-form structures.
【CateGory Index】: P618.13
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