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《Acta Petrolei Sinica》 2012-04
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Main controlling factors and formation models of natural gas reservoirs with high-temperature and overpressure in Yinggehai Basin

XIE Yuhong1 ZHANG Yingzhao1,2 LI Xushen1 ZHU Jiancheng1 TONG Chuanxin1,2 ZHONG Zehong1 ZHOU Jiaxiong1,2 HE Shenglin1(1.Zhanjiang Branch of CNOOC Ltd.,Zhanjiang 524057,China; 2.College of Resources,China University of Geosciences,Wuhan 430074,China)  
There are three main factors that control the formation of productive lithologic gas-reservoirs with high-temperature and overpressure in the first member of the upper Miocene Huangliu Formation in Yinggehai Basin,South China Sea.These three factors are ①a gravity-flow driven sandstone reservoir with high quality;②a gas-reservoir located in the west side of the eastern and western provenance conjunction and overlain by high-quality neritic-facies mudstones as the cap rock;and ③a gas-reservoir located in the diapir outskirt,under which there exists a fault/fissure system connecting with underlying overpressure high-maturity source rocks of the mid-Miocene Meishan Formation and lower Miocene Sanya Formation.High-temperature and overpressure gas reservoirs in Yinggehai Basin have two main gas-accumulating models,one is the lithologic pattern,in which gas reservoirs are distributed in wings and outskirts of the diapir anticline,even in the syncline base,and characterized by the earlier formation of lithologic traps that are consequently uncontrolled by diaper structures,and the other is the anticline pattern,in which gas reservoirs are distributed on the diapir anticline,formed by structures and consequently controlled by diapir structures.Compared with the structural gas reservoir,the lithologic gas reservoir is of good permeability,large-scale reserves and productive capacity.
【Fund】: 国家重大科技专项(2008ZX05023-04)资助
【CateGory Index】: P618.13
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