2001年 Ms 8.1 中央昆地震产生的协同地震冲击滑落和破裂长度
Aiming Lin1, Bihong Fu, Jianming Guo
1Institute of Geosciences, Faculty of Science, Shizuoka University, 836 Ohya, Shizuoka 422-8529, Japan. slin@ipc.shizuoka.ac.jp
概括
2001年中部昆地震造成了创纪录的400公里表面破裂,滑行16.3米. 在昆断层上,这种显著的冲击滑动运动证明了西藏的存在.
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
- 地震学 地震学
背景情况:
- 西藏高原由于印度和欧亚板块之间持续的碰撞而在构造上活跃.
- 了解断层行为对于该地区的地震危险评估至关重要.
研究的目的:
- 为了分析2001年中央昆地震的表面破裂特征.
- 调查地震破裂长度和位移对区域构造学的影响.
主要方法:
- 对地震表面破裂区域的实地调查.
- 分析地震数据以确定地震的强度和特征.
主要成果:
- 中部昆地震 (Ms 8.1) 造成了长约400公里的表面破裂.
- 最大左侧冲击滑动位移达到16.3米,是同地震表面破裂报告的最大位移.
- 该事件发生在西藏北部活跃的昆断层.
结论:
- 广泛的断裂和大位移表明昆断层在适应区域构造力方面发挥了重要作用.
- 地震的特征支持昆断层分裂变形模型,导致西藏向东挤出.
- 这适应了印度板块继续向北透到欧亚板块的情况.
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