A new type of rare earth elements deposit in weathering crust of Permian basalt in western Guizhou, NW China

A new type of rare earth elements (REEs) deposit was discovered from the gaolinite mudstone in the weathering crust of Permian basalt, Bijie region, western Guizhou, China. It contained ∑RE2O3 0.065%-1.086%. This type of REEs deposit was widely distributed with steady horizon and thickness of 3-4 m....

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Bibliographic Details
Published inJournal of rare earths Vol. 26; no. 5; pp. 753 - 759
Main Author 杨瑞东 王伟 张晓东 刘玲 魏怀瑞 鲍淼 王敬欣
Format Journal Article
LanguageEnglish
Published Elsevier B.V 01.10.2008
Guizhou University,Guiyang 550025,China%Research Institute of Science and Technology lnforraatlon,General Research Institute for Non-ferrous Metals,Beijing 1O0O88,China
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Summary:A new type of rare earth elements (REEs) deposit was discovered from the gaolinite mudstone in the weathering crust of Permian basalt, Bijie region, western Guizhou, China. It contained ∑RE2O3 0.065%-1.086%. This type of REEs deposit was widely distributed with steady horizon and thickness of 3-4 m. The ore-bearing weathering crust (kaolinite) of the three discovered REEs deposits belonged to the third episode of the Emeishan basalt eruption. The new type of REEs deposit was suggested that basalt (tuff) weathering could lead to the enrichment of the rare earth elements. Therefore, it is of important economic significance to explore REEs deposits in the weathering crust of basalt (tuffs) in Yunnan, Guizhou, and Sichuan Provinces.
Bibliography:11-2788/TF
basalt (tufts)
upper Pemaian
Guizhou Province
weathering crust
rare earth elements deposits; weathering crust; basalt (tufts); upper Pemaian; Guizhou Province
rare earth elements deposits
P31
ObjectType-Article-2
SourceType-Scholarly Journals-1
ObjectType-Feature-1
content type line 23
ISSN:1002-0721
2509-4963
DOI:10.1016/s1002-0721(08)60177-5