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《Journal of Daqing Petroleum Institute》 2006-05
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Pore evolution model for Xujiahe formation reservoir in West Sichuan foreland basin

WANG Cheng-lin~(1,2),DU Ye-bo~1,ZHANG Jian~3(1.China Petroleum University,Beijing 102249,China;2.Tarim Branch,Research Institute of Petroleum,PetroChina,Beijing 100083,China;3.Basin & Reservoir Research Center,Inf.& Res.School,China Petroleum University,Beijing 102249,China)  
Western Sichuan foreland basin experienced two foreland structure stage: peripheral foreland stage in late-Triassic and intra-continental foreland thrusting in late Cretaceous and Neogene.The reservoir of Western Sichuan foreland basin was closely interconnected with these two stage foreland structure.The structural evolution difference of each foreland belt determined the difference of sedimentation sand bodies and the evolution of reservoir.The reservoir of thrust belt was mainly of pore-fracture type,dissolved pore,fracture and a little primary pore are mainly interstice of the reservoir.Foredeep belt was characterized by secondary pore-fracture reservoir type and dissolved pore.The interstice of foreland slope was mainly dissolved pore and some primary pore. And in forebulge belt mixed aperture of primary pore and dissolved pore was mainly interstice of the reservoir.
【Fund】: 国家“十五”科技攻关项目(2001BA605A-06-02)
【CateGory Index】: P618.13
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