沿南开潜伏区分支的分裂断层沿着南开潜伏区分支
Jin-Oh Park1, Tetsuro Tsuru, Shuichi Kodaira
1Institute for Frontier Research on Earth Evolution, Japan Marine Science and Technology Center, Yokosuka 237-0061, Japan. jopark@jamstec.go.jp
概括
在南开浮带中发现了急剧入的分层断层,起源于板块边界. 这些断层可能在适应8.1级东南海地震带来的压力方面发挥了关键作用.
科学领域:
- 地质物理学 地质物理学
- 地震学 地震学
- 构造学 构造学 构造学 构造学
背景情况:
- 南开潜伏区是一个地震活跃的地区,容易发生大规模地震.
- 了解断层结构对于地震危险评估至关重要.
研究的目的:
- 调查在东南海地震破裂区域存在和特征的splay断层.
- 确定这些断在地震应变适应中的作用.
主要方法:
- 对地震反射形状的分析.
- 识别断层几何形状及其与板边界的关系.
主要成果:
- 在断裂区域中观察到急剧向陆地倾斜的分离断层.
- 这些断层始于板块边界界面,深度约10公里.
- 这些断层延伸到地的上层,从谷轴向陆地.
结论:
- 分裂断层是南开潜流区的一个重要结构特征.
- 在这些活跃的裂纹上滑动是适应弹性应变的潜在机制.
- 这一发现对理解地震破裂过程和地震危险有重要意义.
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