磁堤共振是由非常长周期的地震信号推断出来的
Hiroyuki Kumagai1, Koji Miyakawa, Hiroaki Negishi
1National Research Institute for Earth Science and Disaster Prevention, Tsukuba, Japan. kumagai@bosai.go.jp
概括
在地震群中检测到非常长周期 (VLP) 地震信号. 分析表明,充满了岩的堤产生了共振,产生了这些信号,为火山系统提供了洞察力.
科学领域:
- 地质物理学 地质物理学
- 火山学 火山学是一门学科.
- 地震学 地震学
背景情况:
- 非常长周期 (VLP) 地震信号是低频的地震波.
- 了解VLP信号的源机制对于火山监测至关重要.
研究的目的:
- 为了研究在地震群中观察到的VLP信号的源机制.
- 确定液体填充裂在产生VLP地震活动中的作用.
主要方法:
- 分析VLP信号的周期接近10秒,持续时间约为300秒.
- 源机制分析和波形模拟.
- 应用一个充满流体的裂模型.
主要成果:
- 观察到的VLP信号与Hachijo岛下方的一群地震有关.
- 源机制分析和波形模拟始终表明,充满流体的堤防的共振.
- 该堤被建模为含有玄武岩的岩.
结论:
- 充满岩的堤的共振是观察到的VLP信号的可能来源.
- VLP地震信号可以作为探测火山系统的宝贵工具.
- 这项研究增强了我们对火山内的流体动力学和过程的理解.
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