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《Journal of Chengdu University of Technology(Science & Technology Edition)》 2011-02
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Reservoir characteristics and controlling factors of Shangsi Formation in Dushan,South Guizhou sag

WANG Wen-kai,HOU Ming-cai,LIN Liang-biao,LI Gang State Key Laboratory of Oil and Gas Reservoir Geology and Exploitation,Chengdu University of Technology,Chengdu 610059,China  
The reservoir rocks in Shangsi Formation of Lower Carboniferous in Jiadaozhai of South Guizhou sag are marlstones and crystal powder dolomites,followed by bioclast limestones and dolomitic limestones.The sedimentary environment of Shangsi Formation is from the mixed continental shelf to the open carbonate platform.Based on the slice observation and physical properties of the reservoir in Shangsi Formation,this article indicates that the main reservoir spaces are fractures,followed by intergranular(intragranular) dissolved pores and intercrystalline(dissolved) pores.It is a fractured-porous reservoir with low porosity and low permeability.The development of the reservoir is determined by diagenesis.The cementation,compaction and recrystallization have destroied most original pores,and late-stage dolomitization,dissolution and tectonic disruption have formed many secondary pores and fractures.Because of these,the performance of the reservoir is promoted immensely.
【Fund】: 国家重大专题(2008ZX05005);; 全国油气资源战略选区调查与评价项目(XQ-2007-01)资助
【CateGory Index】: P618.13
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