探测世界上最大的海洋高原:从制造到碰撞
Xiaodian Jiang1, Zheng-Xiang Li2,3, Wei Gong1
1Ocean University of China, China.
National science review
|June 27, 2025
概括
通爪高原的地由于深层岩过程而厚,而不仅仅是表面的岩流. 这种深层的岩入侵和底层形成了高原.
科学领域:
- 地质地质地质地质地质地
- 地质物理学 地质物理学
- 板块构造学是一种板块构造学.
背景情况:
- 通爪高原是地球上最大的海洋高原之一.
- 它的形成机制仍然是科学辩论的主题.
研究的目的:
- 阐明负责构建通爪高原地的主要过程.
- 为了区分深层岩过程与表面火山活动的贡献.
主要方法:
- 对地震和重力数据的分析.
- 岩石样本的地化学分析.
- 地动力学建模地的形成.
主要成果:
- 通爪高原的地非常厚.
- 深层岩入侵和底层是主要的过程.
- 洪水玄武岩在高原的整体地体积中起到了很小的作用.
结论:
- 通爪高原的形成主要是由广泛的深层岩活动驱动的.
- 了解这些过程,可以深入了解大型火山性省份的形成.
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