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.
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.
科学领域:
- 地球科学 地球科学 地球科学
- 地质地质地质地质地质地
- 地质形态学 地质形态学
背景情况:
- 西藏东南部河流系统的演变受到构造学,气候和景观变化的影响.
- 了解这些复杂的相互作用需要对河流切口和沉积物的来源进行详细分析.
研究的目的:
- 重建西藏东南部古代河流系统的进化历史.
- 研究该地区构造学,气候和景观演变之间的相互作用.
主要方法:
- 在中部的金沙河上利用了和阿帕 (U-Th) /He热时计.
- 分析了红河河谷晚奥利古纪-米奥纪沉积物的碎地质和热时代学.
- 采用景观演变建模来模拟河流捕获事件.
主要成果:
- 在18-17万年前和8-7万年前的金沙河峡谷中确定了两个主要的河流切割事件.
- 重建了早期南流河流系统的形成,包括古红河,在早期中期的米奥森.
- 记录了这些系统在中后米欧纪被向西扩张的长江所占领的情况.
结论:
- 西藏东南部河流重组和现代排水模式是构造挤出的结果.
- 河流捕获事件导致了景观演变和生物多样性的同时增加.
- 这项研究突出了地形变化对河流系统的重大影响.
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