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Article Navigation >  PETROLEUM GEOLOGY & EXPERIMENT  > 1999  >  21(4): 285-290
XU Han-lin, SHEN Yang, DING Xiao, XU Jia-wei. STRUCTURAL CHARACTERISTICS OF THE MESO-CENOZOIC BASIN AND RANGE PROVINCE IN SOUTHEAST CHINA[J]. PETROLEUM GEOLOGY & EXPERIMENT, 1999, 21(4): 285-290. doi: 10.11781/sysydz199904285
Citation: XU Han-lin, SHEN Yang, DING Xiao, XU Jia-wei. STRUCTURAL CHARACTERISTICS OF THE MESO-CENOZOIC BASIN AND RANGE PROVINCE IN SOUTHEAST CHINA[J]. PETROLEUM GEOLOGY & EXPERIMENT, 1999, 21(4): 285-290. doi: 10.11781/sysydz199904285
shu

STRUCTURAL CHARACTERISTICS OF THE MESO-CENOZOIC BASIN AND RANGE PROVINCE IN SOUTHEAST CHINA

doi: 10.11781/sysydz199904285
  • 1.

    Hangzhou Institute of Petroleum Geology, CNPC, Hangzhou 310023, China

  • 2. Hefei Polytechnical University, Hefei 230009, China

  • Received Date: 1998-04-01
  • Rev Recd Date: 1999-08-19
  • Publish Date: 1999-10-28
    Abstract
  • Basin and range structure developed during the Meso-Cenozoic period in Southeast China was controlled by those pre-existed fault systems.There are three fault systems in the area with NNE-NE, nearly E-W, NW strikes.Based on the characteristics of the basins, there are three types of basins in the area: graben, listric faults and transform-extension.The characteristics of the basin and range province in Southeast China is shown by longitudinal blocks in S-N and cross zones in E-W.Formation of basin and range province in Southeast China was mainly resulted from geodynamic evolution of west marginal-Pacific tectonic domain, and from collision and squeezing of Indian plate with Euro-Asian continent.

     

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