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印度构造板块的迅速漂移 印度构造板块的迅速漂移
Prakash Kumar1, Xiaohui Yuan, M Ravi Kumar
1National Geophysical Research Institute, Hyderabad 500 007, India.
Nature
|October 19, 2007
概括
印度 印度 印度
科学领域:
- 地质物理学 地质物理学
- 板块构造学是一种板块构造学.
- 地力学是什么?地力学是什么?
背景情况:
- 冈多瓦纳岛的分裂开始于1.4亿年前,导致印度洋的开放.
- 大陆碎片表现出不同的移动性;印度的高速是冈多瓦纳岛遗迹中独一无二的.
- 之前的研究表明,地幔羽毛影响了大陆裂变和随后的板块运动.
研究的目的:
- 调查石质层厚度在确定冈多瓦兰地碎片分离速度方面的作用.
- 为了了解控制印度在裂后迅速向北移动的地力学过程.
主要方法:
- 利用剪切波接收器功能分析来估计石层板厚度.
- 对比印度,非洲,澳大利亚和南极洲的石质层根深度.
主要成果:
- 印度拥有最薄的石化层 (~100公里) 在贡德瓦纳岛碎片中.
- 其他碎片 (南非,澳大利亚,南极洲) 具有显著更厚的岩层根 (180300公里).
结论:
- 印度较薄的石质层可能有助于其在冈瓦那兰分离后的快速移动.
- 地幔羽毛活动可能使印度石化层变薄,通过山脊推力或板块拉力增强移动性.
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