2018年Kīlauea火山的裂喷发和山顶崩塌
C A Neal1, S R Brantley2, L Antolik2
1U.S. Geological Survey, Hawaiian Volcano Observatory, 51 Crater Rim Dr., Hawai'i National Park, Hawaii, HI 96718, USA. tneal@usgs.gov emontgomery-brown@usgs.gov.
概括
2018年Kīlauea火山爆发导致东裂区下部 (LERZ) 的重大活动和峰会崩. 通过先进的监测, 可以预测这次重大火山活动中可能发生的危险事件.
科学领域:
- 地质学
- 火山学
- 地震学
背景情况:
- 2018年Kīlauea火山爆发是200多年来东裂区下部发生的最大火山爆发.
- 它涉及重要的喷发裂活动和山顶上的火山口崩.
研究的目的:
- 详细介绍2018年基拉韦亚火山爆发的过程和后果.
- 突出监测在预测火山风险中的作用.
主要方法:
- 喷发动态的分析,包括裂的范围和岩流量.
- 对地震强度和断层滑动的地震数据的评估.
- 量化山峰崩的体积和释放的能量.
主要成果:
- 喷发裂在LERZ中延伸了6.8公里,覆盖了35.5平方公里的岩.
- 发生6.9级地震, 断层滑落约5米.
- 导致相当于4.7-5.4级地震的崩.
结论:
- 2018年Kīlauea火山爆发涉及大量的LERZ岩流和山峰崩塌.
- 有效的历史观察和监测对于成功预测危险至关重要.
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