在长谷火山火山中,伴随地震的膨胀过程
1Berkeley Seismological Laboratory, University of California, Berkeley, CA 94720, USA. U.S. Geological Survey, Menlo Park, CA 94025, USA.
概括
长谷火山中的异常地震事件表明,火山或热水活动正在引发地震. 这些地震表现出非双对 (NDC) 机制,表明流体压力变化影响断层.
科学领域:
- 地质物理学 地质物理学
- 地震学 地震学
- 火山学 火山学是一门学科.
背景情况:
- 长谷火山中的地震可能受到地下过程的影响.
- 了解地震机制对于评估火山和热水风险至关重要.
研究的目的:
- 为了研究1997年长谷火山中地震群期间地震的地震源机制.
- 为了确定是否存在非双对 (NDC) 机制,并表明特定的地质过程.
主要方法:
- 使用宽带波形的区域地震动量张量确定.
- 从1997年11月的一群地震数据的分析.
主要成果:
- 地震 (Mw 4.6-4.9) 呈现出异常的地震辐射,具有显著的体积元件 (非双对矩张量).
- 观察到的重震扩张表明,由热水或岩过程直接触发.
- 类似的NDC解决方案意味着这些异常事件的共同源流程.
结论:
- 异常地震事件很可能是由高压液体注入或岩石加热引起的应力变化引发的.
- 水热或岩过程在触发长谷火山区地震性方面发挥着直接作用.
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