东喜马拉雅语法向北迁移,由OSL温度计揭示
Georgina E King1, Frédéric Herman2, Benny Guralnik3
1Institute of Earth Surface Dynamics, University of Lausanne, CH-1015 Lausanne, Switzerland. Institute of Geography, University of Cologne, 50923 Cologne, Germany. georgina.king@gmail.com.
概括
山脉侵蚀影响了构造的演变. 新的研究使用光学刺激的发光温度计揭示了东部喜马拉雅山脉的挖掘率的增加,这表明侵蚀迁移,但不是构造反.
科学领域:
- 地质学
- 地形学
- 构造学
背景情况:
- 山的演化受侵蚀和构造活动的影响.
- 将表面过程与构造学联系起来的证据往往依赖于间接的相关性.
- 了解这种关系是解读景观动态的关键.
研究的目的:
- 在东部喜马拉雅语法中量化空间和时间挖掘模式.
- 研究表面过程,特别是侵蚀对构造变形的影响.
- 为了确定侵蚀是否驱动或仅仅是对构造活动的反应.
主要方法:
- 用光学刺激发光 (OSL) 温度计来确定岩石挖掘的日期.
- 分析的重点是东部喜马拉雅语法,特别是南切巴尔瓦 - 吉亚拉时期的顶.
- 挖掘率的空间和时间变化得到量化.
主要成果:
- 在过去的百万年里, 挖掘率在南切巴尔瓦 - 吉拉佩里顶增加了.
- 证据表明帕尔隆河的侵蚀向前扩散.
- 主要的挖掘区域已经向北迁移.
结论:
- 表面过程,如侵蚀,显然影响岩石挖掘率.
- 虽然侵蚀影响了挖掘,但它似乎并没有决定构造变形的位置.
- 这些发现表明了复杂的相互作用, 侵蚀会扩散,
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