黄石岩系统的尖挥发性丰富的帽子
Chenglong Duan1,2, Wenkai Song3, Brandon Schmandt4
1Department of Earth and Planetary Sciences, University of New Mexico, Albuquerque, NM, USA. chenglongduan.nju@gmail.com.
Nature
|April 16, 2025
概括
在黄石
科学领域:
- 地质学
- 火山学
- 地震学
背景情况:
- 火山系统的稳定性取决于岩储存的深度和挥发性排泄.
- 黄石火山有一个上层地的岩储, 但它的深度和属性是不清楚的.
研究的目的:
- 为了限制黄石岩顶部的深度和特性.
- 调查储存库中的挥发性排泄和泡积累的情况.
主要方法:
- 控制源地震成像照亮岩的结构.
- 对P波和P到S波反射进行分析,以推断流体/岩的特性.
- 对地震数据与断层模型和动态模型进行比较.
主要成果:
- 在大约3.8公里深处发现了岩储层的尖反射盖.
- 储盖上含有超临界流体和岩混合物,表明气泡溶解和部分保留.
- 地震估计的气泡体积小部分低于爆发前的条件,这表明气泡有效逃逸.
结论:
- 黄石的岩储备很可能是丰富的水晶和持续的供应.
- 有效的气泡进入水热系统促进了水库的稳定性.
- 目前的状态表明一个稳定的系统与高流的岩挥发物逃到表面.
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