索马里兰裂盆地的地结构和地震异构性
Mohammed Y Ali1, Mohammad Ismaiel2, Ibrahim M Yusuf3
1Department of Earth Sciences, Khalifa University of Science and Technology, Abu Dhabi, UAE. mohammed.ali@ku.ac.ae.
Scientific reports
|October 14, 2023
概括
这项研究揭示了索马里兰.
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
- 石灰岩层结构的结构
背景情况:
- 裂边缘是理解大陆石灰岩层破裂和盆地形成的关键.
- 索马里兰的新生代地下层经历了多次裂变事件,但它的地结构是不太了解的.
研究的目的:
- 调查索马里兰裂盆地的地和上层地幔结构.
- 为了确定地和上层地幔变形的性质和方向.
主要方法:
- 遥感接收器功能分析
- 贝叶斯的反转是贝叶斯的反转.
- 常见的转换点成像技术
- 2D前向重力建模 2D前向重力建模
- 剪切波分裂分析 剪切波分裂分析
主要成果:
- 地的厚度有所不同:南部约37-38公里,中部/北部约21公里,沉积物厚.
- 上层地幔的异质性表明方向与非洲-阿拉伯板块运动保持一致,可能是由于天气层流动.
- 地的异构性揭示了罗纪晚期,奥利戈纪和白纪晚期裂事件的化石变形.
结论:
- 这项研究为索马里兰地中裂相关的延伸应变组织提供了第一个详细的见解.
- 上层地幔的异质性与天气层流动有关,反映了区域板块构造学.
- 多个古老裂变事件在地变形结构上留下了明显的印记.
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