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《Journal of Chengdu University of Technology(Science & Technology Edition)》 2007-03
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Lithological characteristics of dolomite in the Lower Triassic Feixianguan Formation of the NE Sichuan Basin,China

GAO Mei-sheng1,ZHENG Rong-cai1,WEN Hua-guo1,LI Lian-xin2,LI Hong21.State Key Laboratory of Oil and Gas Reservoir Geology and Exploitation,Chengdu University of Technology,Chengdu 610059,China;2.Research Institute of Exploration and Development,Changqing Oil-field Company of CNPC,Xi'an 710021,China;3.Chongqing Gas District of Southwest Oil and Gas Company of CNPC,Chongqing 400021,China  
On the basis of analysing the rock structure and combined with the analysis of strontium isotopes and microelement strontium,the authors study the origin of dolomite reservoir in the Lower Triassic Feixianguan Formation of NE Sichuan Basin and recoglize two kinds of origin types: the penecontemporaneous dolostone and burial dolostone. The burial diagenetic dolostone with multiperiodic metasomatic geneses only of reservoir significance,including two main structure types of oolitic dolostone and crystalline dolostone.Intigrativly analyzing the rock structure of the two kinds of dolostone and the geochemical characheristics of strontium isotope and microelement strontium,the authors divide the diagenesis process of the burial dolomitization into early diagenesis,middle diagenesis and late diagenesis.In every diagenesis stage,though the rock structure of reservoir dolostones is notable different.The geochemical characteristics of strontium isotopes and microelement strontium are very similar,but they are congenetic.This not only shows that the burial dolostone diagenetic fluids are sea source formation water which has much strong composition characteristics of strontium isotope in Triassic seawater,but also reflects that the diagenesis process of multiperiodic burial dolomitization happens in the successional evolving and relatively sealing system.So this is much favorable for reservoir development and gas accumulation.
【CateGory Index】: P588.245
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