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《Journal of Chengdu University of Technology(Science & Technology Edition)》 2012-02
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General situation and prospect evaluation of the shale gas in Wufeng-Longmaxi Formation of Sichuan Basin and surrounding areas

WAN Hong-chen,SUN Wei,LIU Shu-gen,RAN Bo,YE Yue-hao, WANG Shi-yu,LUO Chao,TIAN Meng-na State Key Laboratory of Oil and Gas Reservoir Geology and Exploitation, Chengdu University Technology,Chengdu 610059,China  
In Sichuan Basin and surrounding areas,the mud shale in Wufeng-Longmaxi Formation of Upper Ordovician to Lower Silurian is distributed in Leshan-Longnüsi and the Jialidong paleo-uplift area in the middle of Guizhou,and the thickens increasingly to the north,the south and the east.The thickness of the mud shale is 200~500 m,and the thickness of the black shale has the same distribution trends and the thickness is generally 20~80 m.The fraction of organic carbon(TOC) of the shale is more than 1% in most areas of Sichuan Basin,belonging to sapropelicⅠkerogen,generally Ro2%.The black shale section consists of the sediments of transgression to maximum sea level,and the nowaday buried depth is relatively shallow.The buried depth in the south of Sichuan Basin is 1.5~3 km,that in west of Hubei and the east of Chongqing area is 1.5~3 km.The main target zone of the shale gas is the transitional zone from the east of Sichuan Basin to the west of Hubei and the east of Chongqing area.The buried depth of the shale in this zone is 2~3.5 km,and the front of the Daba mountain is the potential exploration advantageous area in future.
【Fund】: 国土资源部全国油气资源战略选区调查与评价专项(2009GYXQ15)
【CateGory Index】: P618.13
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