洞穴记录揭示了北美最深的峡谷最近的起源
Matthew C Morriss1,2, Nate A Mitchell3, Brian J Yanites3
1Earth Sciences Department, University of Oregon, Eugene, OR 97401.
概括
赫尔斯峡谷是北美最深的峡谷,大约210万年前由于一个重要的排水捕获事件而迅速形成. 这一事件改变了蛇河的路线,导致了快速切割,并塑造了现代河峡.
科学领域:
- 地质形态学 地质形态学
- 构造学地质形态学 构造学地质形态学
- 四年纪地质学四年纪地质学
背景情况:
- 黑尔斯峡谷是北美最深的峡谷,其形成历史尚不清楚.
- 关于峡谷形成的先前假设缺乏直接的地球时间和地形约束.
研究的目的:
- 为了确定Hells Canyon切口的时间和机制.
- 提供了对峡谷形成的第一个直接年龄限制.
- 分析切割过程和河流形状的演变.
主要方法:
- 洞穴结合的河流沉积物的宇宙原核化物约会.
- 河流概况分析.
- 河流切割和排水捕获的数值建模.
主要成果:
- 大规模的排水捕获事件发生在大约2.1 ± 1.0万年前.
- 这次捕获事件启动了快速切割,建立了现代的蛇河路线.
- 切口率显著增加,从~0.01 mm y-1增加到~0.16 mm y-1.
- 从捕获地点远离,形成并降低高度的附属针点.
结论:
- 排水捕获是Hells Canyon快速切割和形成的主要驱动因素.
- 这项研究提供了一个非常有限的例子,说明排水捕获如何塑造主要河流峡谷.
- 这些发现解决了关于Hells Canyon形成的长期问题.
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