在夏威夷基拉韦亚火山的岩引发的缓慢滑动
Benjamin A Brooks1, James Foster, David Sandwell
1School of Ocean and Earth Science and Technology, University of Hawaii, 1680 East-West Road, Honolulu, HI 96822, USA.
概括
最近的一次堤入侵可能引发了基拉韦亚火山的缓慢断层滑动事件 (SSE). 入和背景断层爬行都可能导致这些重大地震事件.
科学领域:
- * 火山学和构造物理学
- * 地测和遥感技术
背景情况:
- * Kilauea火山在其移动的南侧呈现缓慢断层滑动事件 (SSEs).
- *火山入侵和SSE之间的相互作用需要进一步研究.
研究的目的:
- * 为了确定最近的堤入侵是否引发了Kilauea南侧的SSE.
- * 了解在基拉韦亚发生SSE的促成因素 (内在和外在).
主要方法:
- * 综合先进的陆地观测卫星 (ALOS) 卫星雷达干扰度数据用于堤入侵.
- *利用全球定位系统 (GPS) 的连续数据进行地面变形.
- * 模拟的库伦缺陷应力变化来自于世俗变形和堤入侵.
主要成果:
- *入侵后的变形模式与之前的SSEs几乎相同.
- * 堤入侵和世俗变形都显著增加了库伦衰竭应力.
- *以前的SSEs发生在背景变形期间,而不是直接侵入后.
结论:
- *诸如堤入侵之类的外部因素可以触发SSEs.
- * 内部因素,如世俗断层爬行,也会导致SSEs.
- *这两种过程都可能在基拉韦亚的SSEs中发挥作用,突出显示了复杂的断层动态.
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