• 责任者：Wu Shenghua (Key Laboratory of Metallogeny and Mineral Assessment ; MLR ; Institute of Mineral Resources ; Chinese Academy of Geological Sciences ; Beijing 100037 ; China) ; Liu Lanming
• 刊名：Mineral Deposits
• 出版年：2012
• 卷期：31(2)
• 关键词：铅锌矿床 ; lead-zinc deposit ; 流体包裹体 ; fluid inclusions ; 湖南 ; Hunan Province
• 页码：p.216-228
• 图表：6 illus., 1 table, 33 refs.
• 分类号：1001
• issnNo：ISSN0258-7106
• isbnNo：CN11-1965/P

The Chaishan-Shexingping Pb-Zn deposits of Dongpo are located in the distal areas of southeast Qianlishan intrusions and comprise Pb-Zn veinlike, columnar and sheet ore bodies, which have been apparently subjected to the alteration of carbonation and silicification. The fluid inclusions in sphalerite, fluorite, quartz and calcite of the Chaishan-Shexingping Pb-Zn deposits of Dongpo are composed of liquid-rich, gas-rich and daughter mineral-bearing inclusions. The homogenization temperatures of fluid inclusions in these minerals range from 140 ℃ to 395 ℃, with peaks being 350 ℃, 240~260 ℃ and 200~220 ℃, respectively, corresponding to various capture events of hydrothermal fluids in the formation processes of Pb-Zn veins and columns.