在喜马拉雅山脉的orogen同时发生的米奥森延伸和缩短
概括
南藏分离系统对喜马拉雅山脉质结构至关重要,在19-22万年前活跃. 这表明地的延伸和收是中世纪的关键构造过程.
科学领域:
- 地质地质地质地质地质地
- 构造学 构造学 构造学 构造学
- 地质时间学 (Geochronology)
背景情况:
- 南藏分离系统 (STDS) 将喜马拉雅山脉的变态核心与其上层分离.
- 它的发展与地厚化的引力潜在能量差异有关.
研究的目的:
- 用地质年代学数据调查STDS活动时间.
- 了解地延伸和收在米奥森时期喜马拉雅地构造学中的作用.
主要方法:
- 从西藏南部的荣布克山谷采集的岩石样本进行地质时间分析.
- 脱落活动与地加厚事件的相关性.
主要成果:
- 地质年代学数据显示,在1900万至2200万年前,STDS细分活动发生.
- 这一时期与地在更深层的结构层面上显著加厚相吻合.
结论:
- 在显著地加厚的米奥琴时期期间,STDS活跃.
- 在喜马拉雅构造学中,延伸的上层和收的下层之间的脱是显著的.
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