在夏威夷Mauna Loa火山的深裂入侵的压力控制,夏威夷
Falk Amelung1, Sang-Ho Yun, Thomas R Walter
1Rosenstiel School of Marine and Atmospheric Sciences, University of Miami, 4600 Rickenbacker Causeway, Miami, FL 33149, USA. famelung@rsmas.miami.edu
概括
毛纳洛阿火山由于深层岩体而膨胀,表明压力转移控制了岩积累. 这一发现对于了解火山变形和喷发潜力至关重要.
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:
- 夏威夷的毛纳洛阿火山表现出由于浅层入侵和基底地震造成的变形.
- 在较低的火山建筑中扩散的适应仍然不太清楚.
研究的目的:
- 为了研究控制毛纳洛阿山变形的地下过程.
- 了解火山下部的岩积聚机制.
主要方法:
- 使用了干扰度合成光圈雷达 (InSAR) 数据.
- 分析了2002年至2005年间的变形模式.
主要成果:
- 检测到西南裂区域中一个中等深度的,类似堤的岩体的世俗膨胀.
- 观察到岩积聚在裂区的部分,此前没有受到入侵和地震的影响.
结论:
- 地下岩积累受到压力转移的影响.
- 浅堤入侵和基底地震在控制岩通道和积聚区方面发挥着重要作用.
相关概念视频
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