• 责任者：Gui Changjie (School of Earth Sciences and Engineering ; Nanjing University ; Nanjing 210093 ; China) ; Jing Shan
• 刊名：Journal of Geology
• 出版年：2011
• 卷期：35(4)
• 关键词：铅锌矿床 ; lead-zinc deposit ; 栖霞山 ; Qixia Mountains
• 页码：p.395-400
• 图表：4 illus., 2 tables, 12 refs.
• 分类号：1001
• 出版序号：20122400
• issnNo：ISSN1674-3636
• isbnNo：CN32-1796/P

Based on the analysis of the geological properties of the ore deposit, the authors discussed the ore-forming material sources, ore control factors and the genesis of the deposit in combination with the previous study. The ore-forming fluid was composed of ore-bearing hydrothermal fluid from deep source, organic fluid from C-P carbonate rock and meteoric water. The organic fluid played an important role in the precipitation and enrichment of ore forming elements. The ore body was controlled by longitudinal fault (F₂), unconformity surface over and under the structural layers and C-P carbonate rock. It was concluded that in the deep part of the deposit, there was prospecting potential along the extension of longitudinal fault (F₂).