• 责任者：Zhang Sukun (School of Earth Science and Resources ; China University of Geosciences ; Beijing 100083 ; China) ; Zheng Youye
• 刊名：Mineral Deposits
• 出版年：2013
• 卷期：32(3)
• 关键词：钼矿 ; molybdenum ores ; 石英脉型矿床 ; quartz veins type deposit ; 西藏 ; Tibet
• 页码：p.641-648
• 图表：3 illus., 1 table, 49 refs.
• 分类号：1001
• issnNo：ISSN0258-7106
• isbnNo：CN11-1965/P

     The Jigongcun molybdenum deposit, located in the middle of the Gangdese metallogenic belt in Tibet, is a quartz-vein type molybdenum deposit hosted in Qushui granodiorite batholith, with ore bodies controlled by the brittle reverse fault. In order to define the ore-forming time of Jigongcun molybdenum deposit, the authors selected five molybdenite samples for Re-Os isotope analysis. It indicates that the metals of the Jigongcun molybdenum deposit might have had a deep-seated magma source(the lower crust to the upper mantle), which experienced remelting from the delaminated lower crust heated by the mantle.