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SEDIMENTARY CHARACTERISTICS AND BASINAL EVOLUTION OF XIZANG (TIBET) TETHYS IN MESOZOIC ERA
引用本文:余光明,王成善,张哨楠. SEDIMENTARY CHARACTERISTICS AND BASINAL EVOLUTION OF XIZANG (TIBET) TETHYS IN MESOZOIC ERA[J]. 中国科学B辑(英文版), 1990, 0(10)
作者姓名:余光明  王成善  张哨楠
作者单位:Chengdu Institute of Geology and Mineral Resource,Chengdu 610060,PRC,Chengdu College of Geology,Chengdu 610059,PRC,Chengdu College of Geology,Chengdu 610059,PRC
摘    要:Based on the characteristics of stratigraphy sedimentary system and paleotectonics, Xizang (Tibet) Tethys can be classified into nine sedimentary basins. The sedimentary and development characteristics of each basin nicely reveal the plate tectonic framework of Xizang (Tibet). The studies show that the Bangong Lake-Dengen fracture zone is intraplate transform boundary, the active continental margin of the Yarlung Zangbo River is of the nature of "range-arc" boundary, not trench-arc-back-arc basin system.


SEDIMENTARY CHARACTERISTICS AND BASINAL EVOLUTION OF XIZANG (TIBET) TETHYS IN MESOZOIC ERA
YU GUANG-MING. SEDIMENTARY CHARACTERISTICS AND BASINAL EVOLUTION OF XIZANG (TIBET) TETHYS IN MESOZOIC ERA[J]. Science in China(Chemistry), 1990, 0(10)
Authors:YU GUANG-MING
Abstract:Based on the characteristics of stratigraphy sedimentary system and paleotectonics, Xizang (Tibet) Tethys can be classified into nine sedimentary basins. The sedimentary and development characteristics of each basin nicely reveal the plate tectonic framework of Xizang (Tibet). The studies show that the Bangong Lake-Dengen fracture zone is intraplate transform boundary, the active continental margin of the Yarlung Zangbo River is of the nature of "range-arc" boundary, not trench-arc-back-arc basin system.
Keywords:Tethys  transform basin  retro-are basin  depositional system  plate tectonics
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