在Mauna Kea火山下第二次沸引起的深度长期地震
Aaron G Wech1, Weston A Thelen2, Amanda M Thomas3
1U.S. Geological Survey, Alaska Volcano Observatory, Anchorage, AK, USA. awech@usgs.gov.
概括
在休眠火山下的深度长期地震 (DLPs) 可能是冰冷岩的信号, 而不是即将爆发的信号. 这项研究将Mauna Kea的100多万个DLP与岩结晶过程联系起来.
科学领域:
- 火山学
- 地震学
- 地质学
背景情况:
- 深度长期地震 (DLP) 是火山的地震事件,通常在静止的火山上观察到.
- DLP的特点是低频地震波, 起源于地球地深处.
- 它们的确切原因和与火山活动的关系仍在进行研究.
研究的目的:
- 在Mauna Kea火山下, 探究一个独特的, 长期存在的DLP的原因.
- 探索岩结晶过程与DLP生成之间的潜在联系.
- 重新评估DLP活动对火山动荡的影响.
主要方法:
- 在19年的Mauna Kea火山地震数据分析.
- DLP事件频率和特征与岩行为的地质模型的相关性.
- 应用流体动力学和岩石学原理来解释地震观测.
主要成果:
- 在Mauna Kea下方发现了一百万个近周期的DLP.
- DLP序列归因于从结晶,停滞的岩中重复的挥发性排泄.
- 这种被称为"第二沸"的过程被认为是观察到的DLP的主要驱动因素.
结论:
- 这项研究为DLP生成提供了新的解释,将其与岩结晶和挥发性排泄联系起来.
- DLP活动可能通常表明停滞,冷却的岩而不是爆发前的条件.
- 这些发现需要重新评估DLP地震性在火山监测中的解释.
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