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LIN Chang-song, GAO Jin-yao, ZHAO Li-hong, ZHAO Jian-ru. Geophysical features of the western-edge fault zone of the South China Sea and its significance of tectonic geology[J]. Haiyang Xuebao, 2009, 31(2): 97-103.
Citation: LIN Chang-song, GAO Jin-yao, ZHAO Li-hong, ZHAO Jian-ru. Geophysical features of the western-edge fault zone of the South China Sea and its significance of tectonic geology[J]. Haiyang Xuebao, 2009, 31(2): 97-103.

Geophysical features of the western-edge fault zone of the South China Sea and its significance of tectonic geology

  • Received Date: 2007-10-10
  • Rev Recd Date: 2009-03-11
  • The western-edge fault zone of the South China Sea is divided into the southern and northern parts about at 8°N.The main fault of the western-edge fault zone is originated from the Mesozoic basement fault, continuously developed into the Cenozoic, and has dominated the growth of Cenozoic basins nearby it.The non-magnetic, high-density igneous rocks in the fault zone belong to granite intrusion of one period among the Indosinian or Yanshanian Ⅰ, Ⅳ and Ⅴ phases, which is most possibly at the end of the Yanshanian.The main fault of the western-edge fault zone extends through the middle of the Wan'an Basin, and its right-lateral strike-slip activities have induced the marginal depressing and rifting at the east of the Wan'an Basin.
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