• 责任者：Chen Guoyong (Guizhou Bureau of Geology and Mineral Exploration & Development ; Guiyang 550005 ; China) ; Wang Yangen
• 刊名：Guizhou Geology
• 出版年：2011
• 卷期：28(2)
• 关键词：铅锌矿床 ; lead-zinc deposit ; 贵州 ; Guizhou Province
• 页码：p.92-98
• 图表：3 tables, 22 refs.
• 分类号：1001
• issnNo：ISSN1000-5943
• isbnNo：CN52-1059/P

According to the former classification of the lead-zinc deposit, combine with the outcome characters, the metallogenic geologic background as the basis, the metallogenic evaluation as the main line, with deep ore-forming theory, modern and ancient sea floor hydrothermal mineralization theory, divides the output environment into 4 types: geosyncline, platform, orogenic zone and modern continental surface and shallow layer. The lead-zinc deposit in the carbonate rock is the most important, and is the major type in Guizhou Province, 3 kinds of rocks can be the host rock: dolomite, dolomitic limestone and limestone.