The Ore Control Factor of Mingguang Fe Multimetallic Deposit in Tengchong, Yunnan
详细信息
- 责任者：Duan Qiaowen (Honghe Branch ; Yunnan Institute of Geological Engineering Exploration and Design ; Kaiyuan 661600 ; China) ; Li Jinmeng
- 刊名：Yunnan Geology
- 出版年：2013
- 卷期：32(2)
- 关键词：多金属矿床 ; polymetallic ores ; 云南 ; Yunnan Province
- 页码：p.171-173, 149
- 图表：1 illus., 1 table, 3 refs.
- 分类号：1001
- issnNo：ISSN1004-1885
- isbnNo：CN53-1041/P
摘要
The Fe multimetallic deposit is in the contact skarn of lenticular dolomite marble between acid intrusive rock and Kongshuhe Formation,with 6 magnetite ore bodies.It belongs to the Fe deposit of contact metasomatism hydrothermal type.The skarn and metallic oxide are formed by the hydrothermal metasomatism,whereas the sulfide is formed under the middle-low T condition.
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