• 责任者：Tang Juxing (Key Laboratory of Metallogeny and Mineral Resource Assessment ; MLR ; Institute of Mineral Resources ; Chinese Academy of Geological Sciences ; Beijing 100037 ; China) ; Do ji
• 刊名：Acta Geoscientica Sinica
• 出版年：2012
• 卷期：33(4)
• 关键词：成矿系列 ; metallogenic series ; 多金属矿 ; polymetallic ores ; 找矿模式 ; prospecting model ; 西藏 ; Tibet
• 页码：p.393-410
• 图表：3 illus., 3 tables, 63 refs.
• 分类号：1001
• issnNo：ISSN1006-3021
• isbnNo：CN11-3474/P

The Gangdise metallogenic belt is one of the most important continual basements for mineral resources in China.  The Lhasa Terrane （Gangdise magmatic arc, 11143） is one of the most significant third-level （III） metallogenic belts. The result shows that there are five groups of minerogenetic series composed of Pb-Zn-Ag minerogenetic series group related to Hercynian volcanism and rift valley, Cu-Au-Fe-Pb-Zn-Ag-Mo minerogenetic series group related to Indo-Chinese and Yanshanian sedimentation-tectonic magmatism, Cu-Au-Fe-Pb-Zn-Ag-Mo-W-U-salt deposits minerogenetic series group related to Himalayan tectonic magmatism and sedimentation in the Gangdise metallogenic belt, which are composed of six minerogenetic series and ten subseries of ore deposits.