在长江沿线加速的米奥森切口,由向前排水盆扩张驱动
Alexander Rohrmann1, Eric Kirby2, Wolfgang Schwanghart3
1Institute of Geological Sciences, Freie Universität Berlin, Berlin, Germany.
Science advances
|September 8, 2023
概括
河流网络的扩张,而不仅仅是山脉的升起,很可能在米奥生纪期间在西藏高原的长江沿线造成了显著的侵蚀. 这表明较早的升高和与升高相比,侵蚀的时间不同.
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:
- 在米奥琴时期沿着西藏高原东南部的快速河流切割传统上与地形增长有关.
- 最近对湖层的发现表明,河流网络的扩张,而不仅仅是提升,影响了地形沟的迁移.
研究的目的:
- 调查河流网络扩张对河流切口动态的影响.
- 探索长江流域扩张在自中世纪后期以来塑造景观中的作用.
主要方法:
- 利用景观演变模拟来模拟流域扩张及其影响.
- 分析了现代点和河流配置的分布,以验证模拟结果.
主要成果:
- 模拟表明,自中世纪晚期以来,长江流域的扩张可能导致12公里的河流切口.
- 观察到的切口点和河流形状的模式与盆地整合驱动切口的假设一致.
结论:
- 在中新世纪晚期,加快的河流切口可能是由河流捕获和流域整合的侵蚀力增加所驱动的.
- 东西藏可能在中古时代之前已经升高,河流切割速度可能与高原升高脱.
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