• 责任者：Zhao Zhonghai (Geological Survey of Heilongjiang Province ; Harbin 150036 ; China) ; Zheng Weizheng
• 刊名：Mineral Deposits
• 出版年：2012
• 卷期：31(3)
• 关键词：铜矿 ; copper ores ; 金矿 ; gold ores ; 多宝山 ; Duobao Mountains
• 页码：p.601-614
• 图表：6 illus., 4 tables, 29 refs.
• 分类号：1001
• issnNo：ISSN0258-7106
• isbnNo：CN11-1965/P

There are multi-periodic Cu-Au ore-forming processes in Duobaoshan area, Heilongjiang Province, which involve Middle Caledonian, Early Yanshanian, and Late Yanshanian periods. The mineralization and metallogenic regularity of ore deposits formed in these periods are discussed in this paper. The porphyry Cu-Mo-（Au） deposits were mainly generated in Middle Caledonian period, the skarn Cu-Fe-（Au） deposits and Mo-W-Zn deposits were mainly formed in Early Yanshanian period, and the epithermal gold mineralization took place in Late Yanshanian period. These different types of ore deposits are mainly controlled by the Middle Ordovician and Lower Devonian strata and the ring structure associated with the NE-and NW-trending faults.