Genesis of the Kaladawan Fe-Mo ore field in Altyn, Xinjiang, China: Constraints from mineralogy and geochemistry

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• 作者：Cheng-Ming Wang^a ; ^b ; Li Zhang^a ; Hao-Shu Tang^c ; ^{tanghaoshu@163.com} ; Hua-Yong Chen^a ; Xi-Liang Li^d ; Yi Zheng^e ; Deng-Feng Li^a ; ^b ; Jing Fang^a ; ^b ; Lian-Hui Dong^d ; Xun Qu^d
• 关键词：Kaladawan Fe&ndash ; Mo ore field ; Altyn Mountains ; Magnetite geochemistry ; Metallogeny ; NW China
• 刊名：Ore Geology Reviews
• 出版年：2017
• 出版时间：March 2017
• 年：2017
• 卷：81
• 期：part_P2
• 页码：587-601
• 全文大小：4592 K
• 卷排序：81

文摘

A new Fe–Mo field was discovered at Kaladawan in the Altyn Mountains. The skarn minerals have compositions similar to those of typical iron deposits. In-situ Trace elemental features of magnetite indicate a skarn origin. The Mo mineralization and Mo-rich magnetite formed by Mo-rich hydrothermal fluids. The Kaladawan Fe–Mo ore field is a skarn system.