侵入引发了2010年艾亚菲亚拉杰克尔爆发的爆炸性喷发
Freysteinn Sigmundsson1, Sigrún Hreinsdóttir, Andrew Hooper
1Nordic Volcanological Center, Institute of Earth Sciences, University of Iceland, Askja, Sturlugata 7, Reykjavik IS-101, Iceland. fs@hi.is
Nature
|November 19, 2010
概括
冰岛的Eyjafjallajökull火山的火山变形是不寻常的,与单个岩腔无关. 入和复杂的地面运动在喷发之前,有微妙的短期前体.
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.
- 遥感 遥感 遥感 遥感
背景情况:
- 岩室膨胀通常在喷发之前,导致快速通缩.
- 像Eyjafjallajökull这样的适度活跃的火山表现出不太了解的变形风格.
- 2010年埃贾菲亚拉乔库尔火山爆发是火山动荡18年之后发生的.
研究的目的:
- 为了调查2010年埃贾菲亚拉杰库尔火山爆发之前和期间的不寻常变形.
- 了解在中度活跃的火山中引发喷发的地下过程.
- 分析岩入侵,变形和喷发风格之间的关系.
主要方法:
- 全球定位系统 (GPS) 的地质测量.
- 对卫星雷达图像进行干扰度分析.
- 与喷发时间表相关的变形模式的分析.
主要成果:
- 第一次喷发之前的变形很快,但在喷发期间可以忽略不计,这表明岩来自深处.
- 一个约0.05立方公里的岩石入侵在三个月内以复杂的方式生长.
- 在第二次喷发期间,与通胀来源分开的明显的收缩源被确定.
- 埃贾菲亚拉约克尔的行为归因于其偏离悬崖的环境和有限的浅层岩.
结论:
- 埃贾菲亚拉杰克尔的喷发变形偏离了典型模型,这是由深层岩源和复杂的侵入驱动的.
- 火山的离岸设置和地下结构影响其喷发行为.
- 长期的动荡信号可能会在重新唤醒之前出现,但短期的喷发前体可能是微妙的.
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