2018年基拉韦亚火山爆发期间的地震表明了岩粘度
D C Roman1, A Soldati2, D B Dingwell2
1Earth and Planets Laboratory, Carnegie Institution for Science, Washington, DC, USA. droman@carnegiescience.edu.
Nature
|April 8, 2021
概括
地震断层平面的解决方案可以表明岩粘度,有助于预测火山喷发风格. 在Kīlauea的旋转断层平面解决方案表明岩粘度增加,提供了新的喷发前体.
科学领域:
- 地质学
- 火山学
- 病理学
背景情况:
- 岩粘度决定了火山爆发的风格和危险潜力,但通常是在火山爆发后进行测量.
- 预测喷发风格需要识别表明岩粘度的前体.
- 2018年Kīlauea火山爆发表现出不寻常的岩变异性,导致了不可预测的火山爆发动态.
研究的目的:
- 研究地震断层溶液与岩粘度之间的联系.
- 确定预测火山爆发风格的前体.
- 了解岩在喷发期间地震活动中的作用.
主要方法:
- 综合分析地震性和岩气质.
- 检查2018年基拉韦亚火山爆发之前和期间地震的断层平面解决方案.
- 对2018年基拉韦亚喷发产物和早期岩的粘度的实验性确定.
主要成果:
- 2018年基拉韦亚火山爆发期间的地震断层平面解决方案表明压力场旋转90度.
- 这种应力场旋转现象以前只与高粘度喷发有关.
- 确定了诱导局部应力场重定向的特定粘度值.
结论:
- 在地震群中旋转的断层平面溶液是高性岩的早期警告.
- 实时监测断层解决方案的方向可以为即将爆发的风格提供关键的见解.
- 这些发现提供了对多相火山系统的合失效和流动的基本见解.
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