展开旋转构造学和地形演变从局部化节点扩散板块边界对应物展开
Bhaskar Kundu1, Frank Zwaan2,3,4, Batakrushna Senapati5
1Department of Earth and Atmospheric Sciences, NIT Rourkela, Rourkela, 769008, India. rilbhaskar@gmail.com.
Scientific reports
|April 8, 2024
概括
在北极和印度的构造系统中观察到旋转构造板运动. 欧勒旋转极附近的一种入式特征影响了这两个地区的构造学和地形学.
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
- 板块运动学 板块运动学
背景情况:
- 大规模的延伸裂系统在裂轴上呈现逐渐变化的延伸.
- 盘子在欧勒极周围的旋转可以诱导相反侧的收缩,形成旋转构造系统.
研究的目的:
- 介绍一个运动模型,比较北极和印度次大陆的旋转构造设置.
- 研究欧勒极和相关特征对构造系统的影响.
主要方法:
- 开发一个集成地质观测的运动模型.
- 对地形数据的分析.
- 对模拟构造模型结果的重新分析.
主要成果:
- 在北极Gakkel Ridge-Chersky Range系统和印度中部构造区之间发现了旋转构造设置的惊人相似之处.
- 地测和地形分析证实了这两个地区的板块旋转运动.
- 北极板块边界是局部化的,而印度中部构造区则表现出分散的变形.
- 这两个区域的欧勒旋转极都位于类似入器的特征附近.
结论:
- 旋转构造板运动是北极和印度构造系统中的一个重要过程.
- 欧勒极附近的体状特征似乎控制了当今的旋转构造学和地形学.
- 相反的变形风格 (局部化与扩散) 存在,尽管类似的旋转动力学.
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