• 责任者：Pang Ercheng (No.217 Geological Party ; Bureau of Geology Exploration of Shanxi Province ; Datong 030001 ; China) ; Xi Weijie
• 刊名：Acta Geoscientica Sinica
• 出版年：2012
• 卷期：33(5)
• 关键词：钼矿 ; molybdenum ores ; 多金属矿 ; polymetallic ores ; 铼—锇计时 ; Re-Os dating ; 山西 ; Shanxi Province
• 页码：p.787-793
• 图表：3 illus., 1 table, 36 refs.
• 分类号：1001
• issnNo：ISSN1006-3021
• isbnNo：CN11-3474/P

The Tanshang molybdenium-polymetallic deposit in Daixian County of Shanxi Province is one of the most typical ore deposits in Wutai Mountains-Hengshan Mountains polymetallic ore-forming area within the northern part of North China Craton. On the basis of an investigation of the geological features of the deposit, Re-Os isotopic dating was conducted for seven representative molybdenite samples. Thus the isochron age is interpreted as the formation time of the molybdenite, i.e., Mo-polymetallic mineralization occurred in Early Cretaceous.Similar to other Mo deposits in the Wutai Mountains, Hengshan Mountains of the northern part of North China Craton, the Tanshang molybdenium-polymetallic deposit was closely associated with the Yanshanian large-scale tectonic-magmatic activity and related to the thinning of the North China Craton since Mesozoic.