通过地震和变形模式观察埃特纳火山的动态
L Scarfì1, M Aloisi2, G Barberi2
1Istituto Nazionale di Geofisica e Vulcanologia - Osservatorio Etneo, Catania, Italy. luciano.scarfi@ingv.it.
Scientific reports
|August 10, 2023
概括
地质数据揭示了埃特纳火山的内部过程. 地震活动和地面变形与火山喷发相关,这表明岩上升会影响地震和火山管道.
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:
- 地质物理数据对于理解火山动态,特别是应力/应变模式和岩上升对地震性的影响至关重要.
- 意大利南部的埃特纳火山是一个活跃的火山系统,具有复杂的内部过程.
研究的目的:
- 分析埃特纳火山二十年来地震性和地面变形.
- 研究地震事件,地面变形和火山活动之间的关系.
- 为了了解埃特纳火山的长期内部动态.
主要方法:
- 详细分析地震性,包括地震分布和焦点机制.
- 检查地面变形模式 (通胀和通缩).
- 地震和变形数据与火山活动的比较.
主要成果:
- 浅层地震,地面变形和火山活动之间存在直接关系,这些活动往往会在重大喷发之前发生.
- 在5-20公里深处对P轴和T轴的分析表明有一个中央压力源.
- 火山的压力场与区域压力场相互作用并影响.
结论:
- 浅层地震应变释放和地面变形是埃特纳即将爆发的关键指标.
- 一个深处的压力源影响着火山的应力场.
- 火山管道系统对区域压力模式产生重大影响.
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