The Metallogenetic Rule of Liguai Au Multimetallic Deposit in
详细信息
- 责任者：Hu Chengjun (Dali Institute of Geology and Mineral Resources ; Yunnan Exploration Institute of Geology and Mineral Resources ; Dali 671000 ; China) ; Yang Hong
- 刊名：Yunnan Geology
- 出版年：2010
- 卷期：29(3)
- 关键词：多金属矿 ; polymetallic ores ; 金矿 ; gold ores ; 云南 ; Yunnan Province
- 页码：p.273-275
- 图表：1 illus., 3 refs.
- 分类号：1001
- issnNo：ISSN1004-1885
- isbnNo：CN53-1041/P
摘要
///The Au deposit is formed by the further Au enrichment of original rock bed with high Au abundance at advantageous place. The genesis of ore deposit must belong to the low T hydrothermal Au deposit of sedimentary-metamorphic type. According to the comprehensive analysis, this metallogenetic zone has the good metallogenetic condition and potentiality, which will probably become a large scale Au multimetallic metallogenetic zone.