大陆沉积的碎片化正在结束喜马拉雅山脉的地质形成
Xiaofeng Liang1, Yang Chu1, Bo Wan1
1State Key Laboratory of Lithospheric Evolution, Institute of Geology and Geophysics, Chinese Academy of Sciences (CAS), Beijing 100029, China.
Science bulletin
|November 2, 2023
概括
大陆板块的脱离解释了印度-欧亚板块融合的放缓和喜马拉雅山脉土壤形成的结束. 这一由潜水的大陆石化层驱动的过程,涉及碎片分离,减少了板块的拉力.
科学领域:
- 地质物理学 地质物理学
- 构造学 构造学 构造学 构造学
- 地震学 地震学
背景情况:
- 大陆的碰撞通过沉降的石化层拉力维持了orogenesis.
- 大陆板汇聚和碰撞的停止仍在争论中.
研究的目的:
- 调查印度-欧亚板块收速度放缓和停止的原因.
- 在西藏高原下面的图像地幔结构,以了解构造过程.
主要方法:
- 区域地震断层扫描使用前所未有的数据覆盖范围.
- 对地幔过渡区结构的分析.
主要成果:
- 在地幔过渡区识别了多个高速异常.
- 他将这些异常解释为印度大陆板的分离碎片.
- 连接块状板块的脱落,减少了板块的拉力.
结论:
- 碎片式的板块分离导致了印度-欧亚大陆融合的米欧纪放缓.
- 这种机制也解释了西藏南部同期的岩火山活动.
- 石块分离被认为是导致大陆碰撞和喜马拉雅山脉产的终结的最终原因.
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