晚凯诺纪河流重组与构造挤出有关,形成了西藏东南部的现代排水系统

Kai Cao1,2, Guocan Wang1, T Mark Harrison3,4

  • 1Hubei Key Laboratory of Critical Zone Evolution, State Key Laboratory of Geomicrobiology and Environmental Changes, School of Earth Sciences, China University of Geosciences, Wuhan 430074, China.

概括

西藏东南部的构造挤出导致了主要的河流重组. 古老的南流河被长江捕获,塑造了现代的排水和增加生物多样性.

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