黄石火山中的岩-岩积的进展
N Bennington1, A Schultz2, P Bedrosian3
1US Geological Survey, Hawaiian Volcano Observatory, Hilo, HI, USA. nbennington@usgs.gov.
Nature
|January 1, 2025
概括
在黄石
科学领域:
- 地质学
- 火山学
- 地质化学
背景情况:
- 黄石火山是一个巨大的火山系统,以大型火山火山喷发和较小的火山后活动而闻名.
- 之前的地震研究表明,火山口下面有大量的岩石融化,但它的爆发性仍然不确定.
- 由于磁电电阻的敏感性,磁电电流数据对于绘制融化分布至关重要.
研究的目的:
- 通过使用磁度数据,模拟黄石火山口的地岩的电阻结构.
- 为了限制融化分布, 评估大火山爆发的可能性.
- 为了确定灌系统的岩来源和路径.
主要方法:
- 使用磁 (MT) 数据创建黄石地的3D电阻模型.
- 解释电阻变化以推断石岩的存在,分布和融化分数.
- 集成的MT结果与现有的地震和地质数据,以了解岩的动态.
主要成果:
- 石融化物存储在分离的,低融化率的区域,使它们在当前状态下很大程度上无法爆发.
- 位于黄石石东北部的最大的融化储存量与最小的火山火山喷发相当.
- 证据表明,低地的岩岩正在向上迁移, 加热东北岩融化区域.
结论:
- 黄石下面的现有岩石岩没有为形成火山口的大规模喷发做准备.
- 来自更深的岩源的热量和物质转移集中在东北火山区.
- 黄石的未来岩石火山活动很可能集中在东北部.
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