沃顿盆地地震的两个并联平面的同时断裂
1Department of Earth Sciences, University of Oxford, Parks Road, Oxford OX1 3PR, UK.
概括
2000年沃顿盆地地震涉及两个平面的同时破裂,通过一种新的机制来适应构造缩短. 这一事件突显了构造板之间的分散变形区域中显著的应力积累.
科学领域:
- 地质物理学 地质物理学
- 地震学 地震学
- 板块构造学是一种板块构造学.
背景情况:
- 沃顿盆地是印度板块和澳大利亚板块之间分散变形的区域.
- 内板地震可以表现出复杂的破裂行为.
- 了解分散板边界的变形机制对于地震危险评估至关重要.
研究的目的:
- 为了分析2000年沃顿盆地地震的断裂特征.
- 调查其破裂机制对区域构造学的影响.
- 为了理解分散变形区域的应力积累.
主要方法:
- 宽带远程地震数据的分析.
- 地震波形建模以确定破裂特征.
主要成果:
- 时刻7.8级地震由两个同时破裂的次事件组成.
- 这些次事件破裂了两个接近结合的平面,通过这个区域以前未知的机制来适应缩短.
- 化石断裂区域上的较大的子事件表现出高压力下降 (约. 20 MPa) 的压力.
结论:
- 2000年沃顿盆地地震展示了一种独特的破裂模式,可以适应构造缩短.
- 在分布式板形变形的区域中,可以积累和释放大量应力.
- 这一事件为印度-澳大利亚板块边界区域复杂的构造学提供了新的见解.
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