加强一个大大印度的大论点
Jun Meng1, Stuart A Gilder2, Xiaodong Tan3
1State Key Laboratory of Biogeology and Environmental Geology, School of Earth Sciences and Resources, China University of Geosciences Beijing, Beijing 100083, China.
概括
桑丹林部分揭示了交织的早期白纪和旧纪层,而不是连续的序列. 这一发现修订了印度-亚洲碰撞的古地理模型,表明它始于5500万年前.
科学领域:
- 地质地质地质地质地质地
- 古生物学的古生物学
- 地质物理学 地质物理学
背景情况:
- 西藏的桑丹林段对于理解印度-亚洲碰撞至关重要.
- 关于其层和古磁记录的年龄存在不同的解释.
研究的目的:
- 重新评估桑丹林部分的地质年龄和古磁记录.
- 为了完善印度-亚洲碰撞模型的启动.
主要方法:
- 古生物学分析分析 古生物学分析
- 石版检查 石版检查 石版检查
- 古磁数据的获取和解释.
主要成果:
- 桑丹林部分被确定为一个推力复合体,其中有间层的早期白纪 (巴雷米亚-阿尔比亚) 和旧纪层.
- 平面图叠加被推力断层破坏,表明不同年龄的不同构造.
- 古磁数据被重新分配到早期白纪单位.
结论:
- 经过修订的约会支持大印度在很大程度上 (2,0003,000公里).
- 印度-亚洲碰撞被限制在西喜马拉雅山脉的55±5万年前开始.
- 亚洲的南部边缘形成并非归因于连续积累的地形,而是连续的Neotethys板块.
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