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Reservoir characteristics of Longtan Formation shale gas in Huayingshan area，eastern Sichuan Basin

Liu Hu，Cao Tao-tao，Qi Ming-hui，Wang Dong-qiang，Deng Mo，Cao Qing-gu，Cheng Bin，Liao Ze-wen   

  1. 1.Shale Gas Evaluation and Exploration Key Laboratory of Sichuan Province，Chengdu 600091，China; 2.Hunan Provincial Key Laboratory of Shale Gas Resource Utilization，Hunan University of Science and Technology，Xiangtan 411201，China; 3.Wuxi Research Institute of Petroleum Geology，SINOPEC，Wuxi 214126，China; 4.Guangzhou Institute of Geochemistry，CAS，Guangzhou 510640，China
  • Received:2018-07-20 Revised:2018-10-18 Online:2019-01-10

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Abstract: In order to reveal shale gas reservoir characteristics and controlling factors of the Longtan Formation transitional organic-rich shales in Huayingshan area，eastern Sichuan Basin，organic geochemistry，mineral composition，and pore structure parameters were analyzed.The results show that the Longtan Formation shales are characterized by high TOC contents averaged at 3.16%.The kerogen type was mainly type Ⅲ，and the average vitrinite reflectance value is 1.2%，reaching moderate to high maturity stage.The clay mineral is concentrated in the Longtan Formation shale，with an average content of 66.24%，which is mainly composed of I/S mixed layer and illite.The main pore space is composed mainly of interbedded pores related to clay minerals and microcracks，and the organic matter pores are not developed.These shales usually have a high specific surface area and pore volume，with mean values of 27.47m2/g and 0.042cm3/g，respectively，which is approximate to the marine Longmaxi Formation shales in southern China.The specific surface area and pore volume have a negative relationship with TOC content，but have a significant positive relationship with clay mineral content，illustrating inorganic matter pores are the main contributor to shale pore space other than organic matter pores.The micro- to mesopores presenting in I/S mixed layer and meso- to macropores in illite are the main components to construct pore system of shales.

Key words: Maceral composition, TOC, Clay minerals, Reservoir characteristics, Transitional facies, Longtan Formation, Huayingshan area

CLC Number: 

  • TE132.2
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