尼泊尔喜马拉雅山脉orogenic带的U-Pb石年龄的构造学影响
概括
大喜马拉雅岩石起源于非洲,并在古老的土壤发育过程中被安置在贡德瓦纳上. 这挑战了他们起源的传统观点和印度-欧亚洲碰撞期间的构造历史.
科学领域:
- 地质和构造学地质学和构造学
- 地质时间学 (Geochronology)
- 石化学 石化学是一门学科.
背景情况:
- 大喜马拉雅山脉的半沉积岩石传统上被认为是印度盾牌地下室向南推进.
- 这种观点与印度和欧亚大陆之间的纪碰撞有关.
- 之前的模型将大喜马拉雅岩石置于小喜马拉雅岩石下面,即在中生代起源的开始.
研究的目的:
- 重新评估大喜马拉雅半导体岩石的起源和构造历史.
- 为了调查沿着主中心推力线发生的变形和移位的时间.
- 为了测试喜马拉雅山脉的传统模型.
主要方法:
- 来自尼泊尔大喜马拉雅半导体岩石的粒的- (U-Pb) 约会.
- 分析原石的起源和在贡德瓦纳的积累.
- 评价地融入的侵袭和变态时间.
主要成果:
- 石年代测定表明,大喜马拉雅原石起源于在前生代晚期泛非洲原石事件期间的东非原石.
- 在坎布里亚-奥尔多维西亚时代,岩石被积累到北贡德瓦纳,并被地融化入.
- 数据表明,在主中心推力沿线有显著的三级前位移.
结论:
- 作为印度地下室的大喜马拉雅岩石起源的传统模型受到挑战.
- 结构性修复将大喜马拉雅岩石置于小喜马拉雅岩石下面,在中生代原始化之前,似乎有缺陷.
- 大喜马拉雅岩石的变形可能发生在早期的古老生态时期,早于印度-欧亚洲碰撞.
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