在无水固体上方的融化控制了火山弧的位置
Philip C England1, Richard F Katz
1Department of Earth Sciences, South Parks Road, Oxford, OX1 3AN, UK. philip@earth.ox.ac.uk
Nature
|October 9, 2010
概括
在俯冲区的岩分离驱动着地球的化学差异化. 火山弧的位置揭示了融化过程,精确地指出了沟最近的无水固体边界上方的弧.
科学领域:
- 地质化学 地质化学
- 地质物理学 地质物理学
- 石化学 石化学是一门学科.
背景情况:
- 潜伏区的岩分离是地球化学分化的关键.
- 人们对融化形成和上升过程的了解仍然很少.
- 火山弧位置被用来推断潜伏区过程,但解释各不相同.
研究的目的:
- 区分火山弧位置的现有解释.
- 为了阐明融形成和运输在俯冲区的机制.
主要方法:
- 开发了一种现实的热传递在俯冲区的数学模型.
- 从模型中得出一个简单的缩放参数.
- 分析了热结构和融化路径.
主要成果:
- 火山弧的位置并不能通过板块的流体释放来解释.
- 弧形位置与无水固体边界与沟的最接近相对应.
- 从这个区域上升的岩显著改变了地幔的热结构.
结论:
- 火山弧面尖,位于无水固体边界以上.
- 岩热量足以控制到地表的融化途径.
- 这项研究完善了对岩产生和运输在俯冲区的理解.
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