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《Journal of Palaeogeography》 2004-02
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Diagenesis of oolitic bank of the Feixianguan Formation of Lower Triassic in Luojiazhai Gas Field,northeastern Sichuan Province

Su Liping 1,2 Luo Ping 2 Hu Sherong 1 Luo Zhong 1,2 Liu Liuhong 2 Fang Xiaorong 2 1 China University of Mining and Technology, Beijing 100083 2 Key Laboratory of Oil and Gas Reservoir, Research Institute of Petroleum Exploration and Development,CNPC,Beijing 100083  
The Feixianguan gas reservoirs in the Luojiazhai Gas Field, northeastern Sichuan Province, are composed of the porous oolitic dolomites The reservoirs mainly exist in the oolitic bank facies in the carbonate platforms, which were deposited in high energy environment and mainly controlled by tidal action The primary rocks were sparry oolitic limestone and micrite oolitic limestone, but dolomitization destroyed the original sedimentary textures The diageneses which are constructive to the reservoirs are mainly dolomitization and burial dissolution The dolomitization is the base of forming high quality reservoirs Burial dissolution mainly developed inside the primary micropores, the partly filled intergranular porosities and the intercrystal porosities,which furthermore formed lots of enlarged pores,intergranular pores,oolimolds The diageneses which are destructive to the reservoirs are mainly the filling of minerals in secondary pores,the fissures and the dissolved caverns The data of fluid inclusion analysis showed that the filling of minerals mainly happened during the burial period
【CateGory Index】: P534.51
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