• 责任者：Jiao Jian’gang (School of Earth Science and Resources ; Chang’an University ; Xi’an 710054 ; China) ; Lu Hao
• 刊名：Geoscience
• 出版年：2013
• 卷期：27(3)
• 关键词：铜矿 ; copper ores ; 锌矿 ; zinc ores ; 钴矿 ; cobalt ores ; 铼—锇计时 ; Re-Os dating ; 青海 ; Qinghai Province
• 页码：p.577-584
• 图表：8 illus., 2 tables, 31 refs.
• 分类号：1001
• issnNo：ISSN1000-8527
• isbnNo：CN11-2035/P

     color: #222222">Derni massive sulfide Cu(Zn-Co) deposit is mainly wrapped by ophiolite in East Kunlun Mountains, and 8 massive sulfide ores give an isochronal age of (295.5±7.2) Ma by Re-Os isotope. According to the texture and structure of the ores, mineral compositions and various geochemistry data, the genesis of Derni Cu(Zn-Co) ore deposit can be summarized as submarine exhalation-sedimentary mineralization and experienced later hydrothermal superimposition, which is similar to Cyprus-type VMS deposit by tectonic setting and mineral compositions.