在雷尼尔山下面的融和流体从潜水板到表面的路径
R Shane McGary1, Rob L Evans1, Philip E Wannamaker2
1Department of Geology and Geophysics, MS#22, Woods Hole Oceanographic Institution, 360 Woods Hole Road, Woods Hole, Massachusetts 02543, USA.
Nature
|July 18, 2014
概括
这项研究揭示了岩形成和山下登的完整路径. 雷尼耶使用磁数据. 它可视化了从浮导板块释放的流体,地幔融化,以及将岩运输到地储库的流体.
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.
- 构造学 构造学 构造学 构造学
背景情况:
- 收边缘火山运动是由上层地幔部分融化驱动的.
- 融化是通过亚亚压缩解压或由流体诱导的从潜板块流动而发生的.
- 了解岩路径对于评估火山风险至关重要.
研究的目的:
- 在潜水设置中,图像显示流体融化阶段的完整路径.
- 为了研究岩生成和山下登的机制. 雷尼尔. 这是一个.
- 整合地质物理数据,以加强对地下流体和融化动态的限制.
主要方法:
- 美国华盛顿州中部的磁铁电流 (MT) 数据采集.
- 在MT逆转中整合各位的地震研究约束.
- 电导率的3D成像,以划分流体和融化分布.
主要成果:
- 鉴定了从降温板块释放的液体.
- 绘制了流体迁移到上面的地幔的地图.
- 解决了岩在内融化,并将其运送到山下地的地水库. 雷尼尔. 这是一个.
结论:
- 该研究成功地描绘了岩从板块脱水到地储存的整个旅程.
- 结合MT和地震数据,提供了前所未有的细节关于俯冲区的岩管道.
- 这些发现有助于我们更好地理解火山在汇聚边缘的火山过程.
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