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The characteristics and origin of the Hoidas Lake REE Deposit

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The article was published on 2010-01-01 and is currently open access. It has received 11 citations till now. The article focuses on the topics: Allanite.

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Journal ArticleDOI

Geology and market-dependent significance of rare earth element resources

TL;DR: In this paper, the authors proposed that the ideal rare earth element (REE) development targets would be located in a politically stable jurisdiction with a pro-mining disposition such as Canada and Australia.
Journal ArticleDOI

Geochemical Characteristics of Apatite in Heavy REE-rich Deep-Sea Mud from Minami-Torishima Area, Southeastern Japan

TL;DR: In this paper, the authors conducted geochemical and mineralogical investigations of the rare earth and yttrium (REY)-rich mud from the Minami-Torishima area in the Pacific in order to clarify the concentration of REY and their host-phase in the mud.
Book ChapterDOI

REE Mineralogy and Resources

TL;DR: In this article, the potential sources of rare earth elements (REEs) are reviewed, including ion-adsorption types and apatite deposits, which are regarded as the most critical group of elements for the future green technologies.
Book ChapterDOI

The Ore Minerals and Major Ore Deposits of the Rare Earths

TL;DR: This article gave an overview of the major and minor ore minerals of the rare earths, and of the related major ore deposits, and indicated that the apparent dominance of China is economically and politically powered.
Journal ArticleDOI

Hydrothermal evolution in the hoidas lake vein-type ree deposit, saskatchewan, canada: constraints from fluid inclusion microthermometry and evaporate mound analysis

TL;DR: The Hoidas Lake rare earth element (REE) deposit, located in northern Saskatchewan, Canada, is a structurally controlled vein-type LREE deposit with allanite-(Ce) and fluorapatite as the main REE carriers.
References
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Hydroxyl groups in nonmetamict chevkinite-(Ce): a crystal chemical discussion

TL;DR: In this paper, an electrostatic charge balance for chevkinite based on the assigned site-population from chemical data was calculated without the hydrogen contribution, and the resulting empirical bond-valence sum on O6, O8, O2, O3, O5, and O4 ranged from 1.73 to 1.95 vu.
Journal ArticleDOI

Mineralization by mantle fluids in the Miaoniuping REE deposit, Sichuan Province, China

TL;DR: The Miaoniuping REE deposit, Sichuan Province, China is the second largest primary LREE deposit which is a little smaller than the world's largest Bayan Obo REE mine.
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