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    Volume 40 Issue 1
    Jan.  2015
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    Article Navigation >  Earth Science  > 2015  >  40(1): 169-178
    Lin Zhengliang, Wang Hua, Li Hongjing, Ma Qinglin, Li Yuan, Zhao Shu'e, 2015. Genetic Mechanism of Double-Layer Structure in Paleogene of Fushan Sag, Beibu Gulf Basin. Earth Science, 40(1): 169-178. doi: 10.3799/dqkx.2015.012
    Citation: Lin Zhengliang, Wang Hua, Li Hongjing, Ma Qinglin, Li Yuan, Zhao Shu'e, 2015. Genetic Mechanism of Double-Layer Structure in Paleogene of Fushan Sag, Beibu Gulf Basin. Earth Science, 40(1): 169-178. doi: 10.3799/dqkx.2015.012
    shu

    Genetic Mechanism of Double-Layer Structure in Paleogene of Fushan Sag, Beibu Gulf Basin

    doi: 10.3799/dqkx.2015.012
    • 1.

      SINOPEC Geophysical Research Institute, Nanjing 211103, China

    • 2.

      College of Geosciences, China University of Petroleum, Beijing 102249, China

    • 3.

      Faculty of Earth Resources, China University of Geosciences, Wuhan 430074, China

    • 4.

      China Southern Petroleum Exploration and Development Corporation, Guangzhou 510240, China

    • Received Date: 2014-09-03
    • Publish Date: 2015-01-15
      Abstract
    • Based on the regional tectonic analysis of Beibu Gulf basin, in this paper, the tectonic activities of Fushan sag is studied, the dynamic formation mechanism of the sag is discussed, and the formation mechanism of double-layer structure in Paleogene strata of the eastern area is analyzed. It is regarded that Fushan sag was under the dual effect of sinistral strike-slip of Red River fault and clockwise rotation of Hainan uplift. During the deposition period of the third member of Liushagang Formation (Els3), intense horizontal extension occurred during the rotation and pull-apart of the sag, which provided dynamic source for the antithetic faults of the lower tectonic layer in the eastern area. The rapid uplift of Hainan uplift led to the formation of gravity slumping growth faults in the upper tectonic layer. In the Early Oligocene, the intrusive igneous rocks in the second member of Liushagang Formation (Els2) formed a natural barrier. Finally, there formed the double-layer structure. The forming process of the double-layer can be divided into five major stages as follows: rifting embryonic period, extending faulted period of the lower tectonic layer, development period of middle plastic layer, formation period of tectonic system, and finalizing period of double-layer structure.

       

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