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Article Navigation >  PETROLEUM GEOLOGY & EXPERIMENT  > 2014  >  36(2): 194-199
Wang Miao, Huang Chuanyan, Zuo Zongxin, Lin Zhengliang, Wang Baohua. Controls of synsedimentary faults on sedimentary filling of 1st member of Liushagang Formation in Yongan-Bailian areas in Fushan Sag, Beibuwan Basin[J]. PETROLEUM GEOLOGY & EXPERIMENT, 2014, 36(2): 194-199. doi: 10.11781/sysydz201402194
Citation: Wang Miao, Huang Chuanyan, Zuo Zongxin, Lin Zhengliang, Wang Baohua. Controls of synsedimentary faults on sedimentary filling of 1st member of Liushagang Formation in Yongan-Bailian areas in Fushan Sag, Beibuwan Basin[J]. PETROLEUM GEOLOGY & EXPERIMENT, 2014, 36(2): 194-199. doi: 10.11781/sysydz201402194
shu

Controls of synsedimentary faults on sedimentary filling of 1st member of Liushagang Formation in Yongan-Bailian areas in Fushan Sag, Beibuwan Basin

doi: 10.11781/sysydz201402194
  • 1.

    Key Laboratory of Tectonics and Petroleum Resources of Ministry of Education, China University of Geosciences, Wuhan, Hubei 430074, China

  • 2. Wuxi Research Institute of Petroleum Geology, SINOPEC, Wuxi, Jiangsu 214126, China

  • 3. Faculty of Earth Resources, China University of Geosciences, Wuhan, Hubei 430074, China

  • 4. SINOPEC Geophysical Research Institute, Nanjing, Jiangsu 210014, China

  • Received Date: 2013-05-20
  • Rev Recd Date: 2014-01-22
  • Publish Date: 2014-03-28
    Abstract
  • The comprehensive analyses of the sedimentary systems and synsedimentary faults in the 1st member of the Liushagang Formation in the Fushan Sag were made based on high-resolution sequence stratigraphy, sedimentology and structural geology. 3 sedimentary systems were concluded including braided river delta, fan delta and lacustrine sedimentary system. 9 sedimentary microfacies were classified. The synsedimentary systems in the 1st member of the Liushagang Formation in the Yongan-Bailian areas of the Fushan Sag were divided into the western extending accommodation fault system, the eastern strike-slip accommodation fault system and the central transfer fault system. The differential activities of the faults on each side of the central transfer fault system resulted in the migration of formation thickness center, migrating from west to east in the 1st member of the Liusha-gang Formation. The space-time evolution regularities of sedimentary systems indicated that the main delta sand body also migrated from west to east in the 1st member of the Liushagang Formation. The development of synsedimentary faults controlled the distribution of sedimentary systems and 3 controlling patterns were concluded.

     

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