多个水库之间的岩转移对火山爆发周期的影响
Derek Elsworth1, Glen Mattioli, Joshua Taron
1College of Earth and Mineral Sciences, Penn State University, University Park, PA 16802, USA. elsworth@psu.edu
概括
火山爆发是偶尔发生的. 苏弗里埃尔山火山内部的岩转移显示,持续的深层供应为中层地中的水库提供食物,这偶尔会导致表面喷发.
科学领域:
- 火山学 火山学是一门学科.
- 地质物理学 地质物理学
背景情况:
- 火山爆发是偶尔发生的,尽管持续的岩供应.
- 了解岩转移动态对于预测火山爆发至关重要.
研究的目的:
- 为了在Soufrière山火山内的岩转移进行地质图像.
- 调查导致偶尔火山爆发的机制.
主要方法:
- 分析岩外流和表面变形历史.
- 深层地管道的地质成像.
主要成果:
- 观察到来自深层地和地幔的连续岩供应.
- 岩转移发生在一个中层地的储库 (大约. 12公里) 到一个浅水库 (约. 6公里) 的距离.
- 插曲性喷发与浅层水库下面的岩的插曲性"门"有关.
结论:
- 苏弗里埃尔山火山以连续的深层岩供应系统运行.
- 插曲性喷发是通过从中层地水库中插曲性转移岩来控制的.
- 一个概念模型解释了火山周期性通过一个门中间地的岩储.
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