Discussion on the Deposit Features and Genetic Characteristics of Vanadium-Titanium Magnetite <?xml:namespace prefix = st1 ns = "urn:schemas-microsoft-com:office:smarttags" /><st1:State w:st="on">Ore</st1:State> in Xiaohongshan, <st1:place w:st="on">Western Inner Mongolia</st1:place><?xml:namespace prefix = o ns = "urn:schemas-microsoft-com:office:office" /><o:p></o:p>

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Discussion on the Deposit Features and Genetic Characteristics of Vanadium-Titanium Magnetite Ore in Xiaohongshan, Western Inner Mongolia

详细信息

责任者：Yang Fuxin (Institute of 203 Nuclear Research ; Xianyang 712000 ; China) ; Li Weimin
刊名：Northwestern Geology
出版年：2010
卷期：43(3)
关键词：钒钛磁铁矿矿床 ; vanadium titano-magnetite deposit ; 内蒙古 ; Inner Mongolia
页码：p.66-74
图表：7 illus., 4 tables, 9 refs.
分类号：1001
issnNo：ISSN1009-6248
isbnNo：CN61-1149/P

摘要

Xiaohongshan and Damiao vanadium and ilmenite deposits in the Tianshan Mountains-Yinshan belts in the similar latitude. The early Hercynian gabbro rock is the main mine body. The consistent income-based distribution of vanadium-titanium magnetite is shown mostly in the surface, and in the deep is the magma-shaped like layered sub-vanadium-titanium magnetite output. The ore body is stable and rich. The magnetite and ilmenite ore minerals are mainly symbiotic elements such as vanadium, which is a magma-differentiation and segregation-penetration superposition compound type of vanadium-titanium magnetite, and a new type of type between Panzhihua and Damiao V-Ti magnetite-type ore-forming characteristics. The discovery of the type of mineralization has a certain scientific significance for the similar types of vanadium-titanium magnetite.