在1983年夏威夷基拉韦亚火山爆发之前,高岩储存率
1U.S. Geological Survey, 345 Middlefield Road, MS 977, Menlo Park, CA 94025, USA. U.S. Geological Survey, Hawaiian Volcano Observatory, HI 96718, USA.
概括
1975年地震后,基拉韦亚火山的快速变形是由堤扩张和断层爬行驱动的. 这表明岩供应速度是之前估计的两倍,可能引发了1983年的喷发.
科学领域:
- * * 火山学 关于火山的研究
- * * 地质物理学
- * 构造学 构造学 构造学
背景情况:
- * 1975年地震后和1983年火山爆发前, Kilauea火山经历了前所未有的快速变形.
- *以前对岩供应速度的估计可能无法完全解释观察到的变形模式.
研究的目的:
- * 调查驱动基隆火山快速地形变形的机制.
- * 为了估计岩进入基拉韦亚裂区域的岩供应速度.
- * 了解变形,岩储存和1983年火山爆发的开始之间的关系.
主要方法:
- * 火山变形的三维数值建模. 火山变形的三维数值建模.
- *分析变形数据与地震和地质记录相结合.
主要成果:
- * 变形与裂区域的堤扩张和南侧下面的低角度断层爬行一致.
- *估计的岩供应速度为每年0.18立方公里,是之前估计的两倍.
- *在1975年地震之后,高水平的岩储存可能导致了1983年的喷发.
结论:
- * 1975年的地震显著改变了基拉韦亚的变形模式.
- * 增强的岩供应和储存是基拉韦亚火山喷发周期的关键因素.
- * 数字建模为火山过程提供了关键的见解.
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