Trace Elements Characteristics of the Tectonites and Tectonogeochemical Exploration Model for the Shizishan Copper Deposit in oft-com:office:smarttags" />Yimen , Yunnan
详细信息
- 责任者：Li Qiang (Faculty of Land Resource Engineering ; Kunming University of Science and Technology ; Kunming 650093 ; China) ; Han Runsheng
- 刊名：Geotectonica et Metallogenia
- 出版年：2011
- 卷期：35(1)
- 关键词：铜矿 ; copper ores ; 构造地球化学 ; tectono-geochemistry ; 云南 ; Yunnan Province
- 页码：p.149-155
- 图表：5 illus., 5 tabels, 16 refs.
- 分类号：1001
- issnNo：ISSN1001-1552
- isbnNo：CN44-1595/P
摘要
The Shizishan copper deposit located inside the Yimen rift basin of Kuanyang Rift is a medium sized sedimentary-reformation type copper deposit. The main ore-bodies are hosted in the Luoxue Formation dolostone and constrained by the Shizishan anticline and NE-trending compresso-shear faults. Tectono-geochemical investigation shows that the fault zone is intensively mineralized,and the ore metals such as Cu, Bi, Mo, Co, Mn, Ag, Pb are especially enriched in the tectonites. The geochemical exploration model suggests that the area in-between the No.3 and No.8 exploration line is likely the most potential target for ore-bodies at depth.
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