• 责任者：Jiang Yongguo (Faculty of Land Resource Engineering ; Kunming University of Sciences and Technology ; Kunming 650093 ; China) ; Cui Yinliang
• 刊名：Mineral Resources and Geology
• 出版年：2011
• 卷期：25(5)
• 关键词：铅锌矿床 ; lead-zinc deposit ; 稳定同位素 ; stable isotopes ; 同位素地球化学 ; isotope geochemistry ; 云南 ; Yunnan Province
• 页码：p.417-422
• 图表：3 illus., 5 tables, 2 refs.
• 分类号：1001
• issnNo：ISSN1001-5663
• isbnNo：CN45-1174/TD

Northeast Yunnan Province is one of the important lead and zinc ore accumulative zones while Yuhucun lead-zinc deposit is one of the ore containing stratum in Yuhucun Formation in the region. The conclusion is that lead-zinc deposit’s composition came from multiple-source and the formative processes was multi-period and multi-stage according to the research on Pb isotope, S isotope and H-O isotope of lead-zinc deposit in Yuhucun Formation in Northeast Yunnan Province. Pb came mostly from earth crust with a small amount coming from the mantle and orogenic belt. S originated from marine with a small amount from biological action. The main metallogenic fluid came from meteorological water and a small amount maybe came from Magmatic water.