- 责任者：Lü Changliang (Faculty of Land Resources Engineering ; Kunming University of Sciences and Technology ; Kunming 650095 ; China) ; Deng Mingguo
- 刊名：Contributions to Geology and Mineral Resources Research
- 出版年：2013
- 卷期：28(4)
- 关键词：铅锌矿床 ; lead-zinc deposit ; 云南 ; Yunnan Province
- 页码：p.529-534
- 图表：6 illus., 1 table, 12 refs.
- 分类号：1001
- issnNo：ISSN1001-1412
- isbnNo：CN12-1131/P
Luziyuan Pb-Zn deposit in, Zhenkang Town, Yunnan Province is asuper-large polymetallic de- posit discovered in recent years. The ore body mainly occurs in Upper Cambrian Shahechang formation and is controlled by NE faults and the associated sub-structures. Spatially, the ore bodies are plunged and distributed in equal distance. Wall rock alterations are developed. Mineralization is dived into meso-epi- thermal stage and mesothermal-high temperature stage. Where marblization, skarnization, pyritization, silicification are developed and overprinted mineralization is strong. Ore materials are mainly derived from the ore-bearing strata and the deeply seated intrusive body. Based on study on lithologies of ore-bearing strata, the ore-control fracture, wall rock alteration and the ore fabric, the deposit is related to multi- staged tectonic movement and magmatic hydrothermal fluid and is a hydrothermal-skarn type Pb-Zn-Fe polymetallic deposit.