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ZHU He-lin, ZHANG Xue-jun, XIE Shi-wen, et al. Sequence Stratigraphy and Its Effect on Reservoir in Xiaqiulitage Formation in Bachu Area, Tarim Basin[J]. Northwestern Geology, 2011, 44(4): 89-96.
Citation: ZHU He-lin, ZHANG Xue-jun, XIE Shi-wen, et al. Sequence Stratigraphy and Its Effect on Reservoir in Xiaqiulitage Formation in Bachu Area, Tarim Basin[J]. Northwestern Geology, 2011, 44(4): 89-96.
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Sequence Stratigraphy and Its Effect on Reservoir in Xiaqiulitage Formation in Bachu Area, Tarim Basin

  • 1.

    State Key Laboratory of Oil and Gas Reservoir Geology and Exploitation, Chengdu University of Technology, Chengdu 610059, China

  • 2.

    Research Institute of Petroleum Exploration and Exploitation in Henan, Nanyang 473132, China

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  • Received Date: April 11, 2011
  • Revised Date: May 22, 2011
  • Published Date: December 04, 2011
    Graphical Abstract
    • Abstract
  • The Upper Cambrian Xiaqiulitage Formation in Tarim Basin has widely developed thick dolomite on restricted platform,and has become the most important reservoir.According to the multidisciplinary analysis of the data on wells and seismic,the Upper Cambrian Xiaqiulitage Formation is divided into four sequence stratigraphic units in Bachu area.The sequence stratigraphic units were charactered by TST and HST.The HST does not develop completely.On the multidisciplinary analysis of lithologic character of dolomite and indication of oil and gas on wells,the sequence stratigraphic units have vital effect on dolomite reservoir.The karstic dolomite reservoir mainly developed in the HST of sequence stratigraphic,especially in the last period of HST with exposition.
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