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Article Navigation >  PETROLEUM GEOLOGY & EXPERIMENT  > 2017  >  39(1): 58-64
Chen Xianliang, Ji Youliang, Yang Keming. Sequence characteristics of the fourth member of Xujiahe Formation in the middle area of Western Sichuan Depression, Sichuan Basin[J]. PETROLEUM GEOLOGY & EXPERIMENT, 2017, 39(1): 58-64. doi: 10.11781/sysydz201701058
Citation: Chen Xianliang, Ji Youliang, Yang Keming. Sequence characteristics of the fourth member of Xujiahe Formation in the middle area of Western Sichuan Depression, Sichuan Basin[J]. PETROLEUM GEOLOGY & EXPERIMENT, 2017, 39(1): 58-64. doi: 10.11781/sysydz201701058
shu

Sequence characteristics of the fourth member of Xujiahe Formation in the middle area of Western Sichuan Depression, Sichuan Basin

doi: 10.11781/sysydz201701058
  • 1.

    College of Geology & Environment, Xi'an University of Science and Technology, Xi'an, Shaanxi 710054, China

  • 2. College of Geoscience, China University of Petroleum, Beijing 102249, China

  • 3. SINOPEC Southwest Oil & Gas Company, Chengdu, Sichuan 610016, China

  • Received Date: 2016-03-24
  • Rev Recd Date: 2016-11-09
  • Publish Date: 2017-01-28
    Abstract
  • The sequence characteristics of the fourth member of Xujiahe Formation in the middle area of Western Sichuan Depression have been studied by using outcrop, core, logging and seismic data. The fourth member of Xujiahe Formation is a three-order sequence and was divided into lowstand system tract, transgressive system tract and highstand system tract. An isochronous sequence stratigraphic framework was established, and its internal sedimentary characteristics were clarified, mainly developing an alluvial fan-alluvial plain-delta-lacustrine depositional system. The sequence was divided into three types based on depositional settings: symmetrical type, asymmetrical type A1 and A2. Type A1 developed in the piedmont region before the Longmen Mountain, the type A2 mainly developed in Zhongjiang-Luodai area, and the symmetrical type mainly developed in the piedmont region before the Longmen Mountain and the depression between Zhongjiang and Luodai. LST and HST of the asymmetric type and symmetric type A2 sequence were advantageous for the development of high-quality reservoirs.

     

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