异常的p波延迟在热泉 - 清晰湖地热区,加利福尼亚州
概括
哈纳山和海山附近的地震波延迟表明存在深层的岩腔. 这些发现表明,在Clear Lake火山场的潜在火山活动和地热能洞察力.
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.
- 地热能源 地热能源
背景情况:
- 远距离地震延迟表明地表下存在异常.
- 克莱尔湖火山田和热泉是已知的地热和火山地区.
研究的目的:
- 为了调查清湖火山场显著的远震延迟的原因.
- 为了了解汉娜山和热泉地热区下的地下结构.
主要方法:
- 对远地震波的行程时间进行分析.
- 对地震延迟场的解释.
主要成果:
- 在汉娜山和泉附近观察到超过1秒的远震延迟.
- 在火山岩和蒸汽储存库中,有一个0.5秒的一般延迟场.
- 延迟延伸到至少20公里的深度.
结论:
- 在汉娜山下面,可能存在一个带有化的核心的岩腔.
- 一个高度破碎的地热水库,可能由部分化的岩石构成底层,被推断为The Geysers.
- 这些深层结构解释了观测到的地震波延迟.
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