Volume 45 Issue 2
Feb.  2020
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Yang Shuo, Wang Wei, Zhang Li, Luo Dingwen, Zou Huayao, 2020. Control Factors and Distribution of Chlorite-Cemented Facies in the Xujiahe Sandstone, Yuanba and Tongnanba Area. Earth Science, 45(2): 479-488. doi: 10.3799/dqkx.2019.011
Citation: Yang Shuo, Wang Wei, Zhang Li, Luo Dingwen, Zou Huayao, 2020. Control Factors and Distribution of Chlorite-Cemented Facies in the Xujiahe Sandstone, Yuanba and Tongnanba Area. Earth Science, 45(2): 479-488. doi: 10.3799/dqkx.2019.011
shu

Control Factors and Distribution of Chlorite-Cemented Facies in the Xujiahe Sandstone, Yuanba and Tongnanba Area

doi: 10.3799/dqkx.2019.011
  • 1.

    College of Geosciences, State Key Laboratory of Petroleum Resources and Prospecting, China University of Petroleum(Beijing), Beijing 102249, China

  • 2.

    CNOOC, Research Institute Ltd., Beijing 100028, China

  • 3.

    SINOPEC Exploration Company, Chengdu 610041, China

  • Received Date: 2019-05-25
  • Publish Date: 2020-02-15
    Abstract
  • The sandstones reservoirs of the Xujiahe Formation in the Yuanba and Tongnanba area, Sichuan Basin have poor qualities, and only those with chlorite rim, which has a content of more than 1.5% (i.e. chlorite-cemented facies) show a higher porosity. Based on lithology and well-logging geology, composition and control factors of formation of sandstones with chloritecemented facies are analysed with thin section analysis, scanning electron microscopic analysis and grain size analysis, well log responses and distribution of sandstones with chlorite-cemented facies are identified with thin section and well logging data. The formation of chlorite rim has strong environmental specificity and sandstone composition selectivity, that is, it develops in the sandstones with good original porosity in the subaqueous distributary channel. Sandstone with chlorite-cemented facies has higher texture maturity and composition maturity, with lower contents of matrix and plastic rock fragment, and it also has a certain amount of volcanic rock fragments (2%~6%). Lower contents of matrix and plastic rock fragment provided space for precipitation of chlorite, and volcanic rock fragments provided source of chlorite precipitation.

     

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