破裂和构造压力导致超快的岩流入堤
Freysteinn Sigmundsson1, Michelle Parks2, Halldór Geirsson1
1Nordic Volcanological Center, Institute and Faculty of Earth Sciences, University of Iceland, IS-102 Reykjavik, Iceland.
概括
如果一个大通道打开,压力增加, 巨大的岩入侵堤可能会发生. 这就解释了岩的快速流动和潜在的喷发危险.
科学领域:
- 地质学
- 火山学
- 地质学
背景情况:
- 巨大的堤群体表明大量的横向岩流, 通常超过数百公里.
- 对于危险评估至关重要的是要了解推动岩迅速沉积的机制.
研究的目的:
- 解释了大规模岩流入堤的条件.
- 在最近的堤入侵中观察到的快速初始岩流速.
主要方法:
- 在堤内的流动力学的数值建模.
- 在堤路径上积累压力的分析.
- 关于2023年11月格林达维克入侵事件的案例研究.
主要成果:
- 如果一个大通道打开,拉伸应力逐渐建立,巨大的岩流入堤是可能的.
- 模拟的初始流量达到每秒大约7400立方米的堤~15公里长.
- 格林达维克的入是这一过程的一个关键例子.
结论:
- 这项研究提供了快速堤传播和大规模岩流动的机制.
- 高流速的入侵构成重大危险,可能导致表面喷发.
- 发现提供了关于大堤的形成和相关火山风险的见解.
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