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《Journal of Chengdu University of Technology(Science & Technology Edition)》 2009-01
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Origin of syndepositional karst reservoir of the Upper Ordovician Lianglitage Formation in the west of Center Tarim Basin,China

LI Ling1,TAN Xiu-cheng1,CHEN Jing-shan1,ZHOU Yan,LIU Hong,WANG Zhen-yu1Resource and Environment Institute,Southwest Petroleum University,Chengdu 610500,China  
The formation of a carbonate reservoir is mainly controlled by such factors as deposition,diagenesis,and structure.Based on this opinion and the basic data as core,thin slick,reservoir property and geomorphic features,the authors analyse the characteristics and origin of the limestone reservoirs of the Upper Ordovician Lianglitage Formation in the west of Center Tarim Basin.In study area,the reservoirs in the Lianglitage Formation mainly exist in the grain limestone bank of the carbonate platform margin.The main reservoir spaces involve the intragranular solution pore,moldilic pore,non-textural solution pore,cave as well as tectonic fissure.The reservoir types belong to that of low-porosity and low-permeability.According to the analyses of the infusion thin slick,diagenesis texture characteristics and microelements and C-O isotopes,such opinion is presented that the dissolution space is correlated with syngenesis karst,and the meteorological water-diagenesis lens in grain limestone bank on the platform margin are the favorable locations of reservoirs.
【Fund】: 中国石油天然气集团公司中青年创新基金项目(06E1018);; 四川省重点学科建设项目(SZD0414)
【CateGory Index】: P618.13
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