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Temporo-Spatial Distribution of Rare Metal and REE Deposits in Xinjiang, Northwest China
引用本文:CHEN Fuwen,LI Huaqin and LU YuanfaOpen Laboratory for Isotopic Geochemistry,China Geological Survey,Yichang,Hubei. Temporo-Spatial Distribution of Rare Metal and REE Deposits in Xinjiang, Northwest China[J]. 《地质学报》英文版, 2002, 76(4): 478-487. DOI: 10.1111/j.1755-6724.2002.tb00101.x
作者姓名:CHEN Fuwen  LI Huaqin and LU YuanfaOpen Laboratory for Isotopic Geochemistry  China Geological Survey  Yichang  Hubei
作者单位:CHEN Fuwen,LI Huaqin and LU YuanfaOpen Laboratory for Isotopic Geochemistry,China Geological Survey,Yichang,Hubei 443003
摘    要:
Many rare metal and REE deposits have been found in the Altay orogenic belt, on the northern margin of the Tarim massif and in the Kunlun-Altun orogenic belt, constituting three very important rare metal-REE mineralization belts in western China. These deposits belong to various genetic types with complex ore-forming mechanism, and were formed in certain mineralization epochs. On the basis of a systematic sum-up of geologic and geochemical achievements and 40Ar-39Ar ages of potassium-rich minerals as well as whole-rock Rb-Sr dating results, the authors systematically analyzed the spatial distribution and mineralization epochs of rare metal-REE deposits in Xinjiang, northwestern China, and concluded that although the Hercynian rare metal-REE mineralizations in this area are very important, pre- and post-Hercynian (especially Indosinian and early Yanshanian) rare metal-REE mineralizations also have important theoretical and economic significance.


Temporo-Spatial Distribution of Rare Metal and REE Deposits in Xinjiang, Northwest China
CHEN Fuwen,LI Huaqin and LU YuanfaOpen Laboratory for Isotopic Geochemistry,China Geological Survey,Yichang,Hubei. Temporo-Spatial Distribution of Rare Metal and REE Deposits in Xinjiang, Northwest China[J]. Acta Geologica Sinica (English Edition), 2002, 76(4): 478-487. DOI: 10.1111/j.1755-6724.2002.tb00101.x
Authors:CHEN Fuwen  LI Huaqin  LU YuanfaOpen Laboratory for Isotopic Geochemistry  China Geological Survey  Yichang  Hubei
Abstract:
Many rare metal and REE deposits have been found in the Altay orogenic belt, on the northern margin of the Tarim massif and in the Kunlun-Altun orogenic belt, constituting three very important rare metal-REE mineralization belts in western China. These deposits belong to various genetic types with complex ore-forming mechanism, and were formed in certain mineralization epochs. On the basis of a systematic sum-up of geologic and geochemical achievements and 40Ar-39Ar ages of potassium-rich minerals as well as whole-rock Rb-Sr dating results, the authors systematically analyzed the spatial distribution and mineralization epochs of rare metal-REE deposits in Xinjiang, northwestern China, and concluded that although the Hercynian rare metal-REE mineralizations in this area are very important, pre- and post-Hercynian (especially Indosinian and early Yanshanian) rare metal-REE mineralizations also have important theoretical and economic significance.
Keywords:rare metal-REE deposits   spatial distribution   temporal distribution   Xinjiang
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