与奈萨/马拉维裂相关的压力动态:对当今东非裂系统动态的含义
Athanas S Macheyeki1,2, Hassan Mdala3
1Department of Geology, College of Earth Sciences and Engineering, the University of Dodoma, Tanzania.
Heliyon
|October 9, 2023
概括
奈萨/马拉维裂表现出横向的力量,其延伸从中心的辐射变化到南部的NNE-SSW. 这条裂主要显示了整个石质层的正常断层与冲击滑动组件.
科学领域:
- 构造学 构造学 构造学 构造学
- 结构地质学 结构地质学
- 地质物理学 地质物理学
背景情况:
- 尼萨萨/马拉维裂 (NMR) 被认为是转变断层或正常断层裂结构.
- 显著的地震活动和低质量的岩存在是NMR的特征,促使人们对其应力动力学进行调查.
研究的目的:
- 为了解决围绕纳萨/马拉维裂应力动力学的争议.
- 分析古压力和断层滑动数据,以了解裂的构造机制.
主要方法:
- 在中部至南部的NMR中使用断层滑坡数据收集进行古压力分析.
- 整合收集的数据与来自裂内的焦点机制的已公布的动力学数据.
主要成果:
- 中央的NMR显示了辐射或亚辐射延伸.
- 南部的NMR经历了倾斜的NNE-SSW横移的构造力,主要是北向南的开口.
- 断层分析揭示了NW-SE趋势断层的左侧运动和SW-dipping断层的右侧运动,表明正常的断层制度具有显著的冲击滑动组件.
结论:
- 核磁共振主要在正常故障状态下运行,其中包含一个实质性的冲击滑动元件,解释了观察到的斜动力学.
- 已识别的构造机制在石层层级上运作,影响地和上层地幔.
- 延伸方向和应力轴从裂的中部到南部有很大差异.
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