• 责任者：Cao Liang (Wuhan Center ; China Geological Survey ; Wuhan 430205 ; China) ; Duan Qifa
• 刊名：Geology and Mineral Resources of South China
• 出版年：2013
• 卷期：29(4)
• 关键词：铅锌矿床 ; lead-zinc deposit ; 扬子地区 ; Yangtze Region
• 页码：p.308-317
• 图表：8 illus., 1 table, 21 refs.
• 分类号：1001
• issnNo：ISSN1007-3701
• isbnNo：CN42-1417/P

     Lead-zinc deposits were widespread in upper Yangtze plate and periphery area. All these deposits, which distributed in Sinian-Qrdovician marine carbonate rocks, controlled by lithology and fault system, main- ly have stratiform and stratoid structure, variable metallogenic temperature, mineralized fluid are hydrothermal brine with high salinity,have special metallogenic setting and ore-forming conditions, have a similar and differ- ent characteristics with MVT lead-zinc deposit. The sedimentary-hosted lead-zinc epigenetic deposits with above characters are defined as Yangtze type lead-zinc deposits. Since the whole country survey in land and resource, significant progress has been made in Yangtze type lead-zinc deposits exploration in recent years. The prospecting work has accumulated proven lead and zinc resources of 10 million tons. To summarize the metallogenic regularity and prospecting criteria of Yangtze type lead-zinc deposits has great signification for further research.