在日本熊本发生的2016年7.1级地震中,阿索火山停止了地震爆发
A Lin1, T Satsukawa1, M Wang1
1Department of Geophysics, Graduate School of Science, Kyoto University, Kyoto 606-8502, Japan.
概括
2016年熊本地震造成了40公里的地表断裂. 在阿索火山口由于岩而停止破裂, 凸显了潜在的火山危险.
科学领域:
- 地质学
- 地震学
- 火山学
背景情况:
- 2016年熊本地震 (Mw 7.1) 发生在日本九州岛.
- 观察到与地震相关的表面破裂.
- 亚索火山是该地区的一个突出的火山特征.
研究的目的:
- 调查2016年熊本地震表面破裂的特征和程度.
- 了解控制地震破裂传播的因素.
- 评估阿索火山对火山危险的影响.
主要方法:
- 对表面破裂进行实地调查.
- 对地震数据的分析.
- 在阿索火山周围进行地质测绘.
主要成果:
- 在Hinagu-Futagawa撞击滑动断层区域和新发现的断层上发现了长约40公里的表面破裂区域.
- 地震表面破裂延伸到阿索火山口,影响火山,但在其中结束.
- 由于阿索火山集团下面存在着岩, 裂变向东北传播停止.
结论:
- 2016年熊本地震的破裂动态受到阿索火山底层的岩系统的影响.
- 卡尔德拉内部断层的终结表明地震活动与火山过程之间存在复杂的相互作用.
- 鉴于发现的地震断层,需要重新评估阿索火山附近的火山风险.
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