Magmatic-hydrothermal fluids

被引：0

作者：

Audétat A. ^{[1
]}

Edmonds M. ^{[2
]}

机构：

[1] Bayerisches Geoinstitut University of Bayreuth, Bayreuth

[2] University of Cambridge, Department of Earth Sciences, Downing Street, Cambridge

来源：

| 1600年 / Mineralogical Society of America卷 / 16期

关键词：

Brecciation; Fluid inclusions; Magma degassing; Magmatic-hydrothermal; Metal precipitation; Ore deposits;

D O I：

10.2138/GSELEMENTS.16.6.401

中图分类号：

学科分类号：

摘要：

Magmatic-hydrothermal fluids play a key role in a variety of geological processes, including volcanic eruptions and the formation of ore deposits whose metal content is derived from magmas and transported to the site of ore deposition by means of hydrothermal fluids. Here, we explain the causes and consequences of fluid saturation in magmas, the corresponding fluid-phase equilibria, and the behavior of metals and ligands during the transition from magma to an exsolved hydrothermal fluid. Much of what we know about magmatic-hydrothermal systems stems from the study of fluid inclusions, which are minute droplets of fluids trapped within minerals during mineral growth. © 2020 Mineralogical Society of America. All rights reserved.

引用

页码：401 / 406

页数：5

共 32 条

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