Hydrothermal Mobilisation of the Rare Earth Elements - a Tale of "Ceria" and "Yttria"

被引：405

作者：

Williams-Jones, Anthony E. ^{[1
]}

Migdisov, Artashes A. ^{[1
]}

Samson, Iain M. ^{[2
]}

机构：

[1] McGill Univ, Dept Earth & Planetary Sci, Montreal, PQ H3A 2A7, Canada

[2] Univ Windsor, Dept Earth & Environm Sci, Windsor, ON N9B 3P4, Canada

来源：

ELEMENTS | 2012年 / 8卷 / 05期

基金：

加拿大自然科学与工程研究理事会;

关键词：

REE; hydrothermal; solubility; speciation; ore formation; AQUEOUS GEOCHEMISTRY; FLUID INCLUSION; INNER-MONGOLIA; NEW-MEXICO; REE; DEPOSIT; COMPLEXES; SALTS; MINERALIZATION; TEMPERATURES;

D O I：

10.2113/gselements.8.5.355

中图分类号：

P3 [地球物理学]; P59 [地球化学];

学科分类号：

0708 ; 070902 ;

摘要：

Although the rare earth elements have been thought by many to be immobile in hydrothermal fluids, we have known since the first attempts to separate them in the early nineteenth century that they are soluble in aqueous solutions. Driven by a need to isolate individual REEs for industrial applications, and more recently to explore for them, we have started to develop an understanding of their solubility and speciation in hydrothermal fluids. This knowledge is allowing us to understand the processes that promote their transport in the Earth's crust, their concentration, and their fractionation.

引用

页码：355 / 360

页数：6

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