• 责任者：Mao Jingwen (Key Laboratory of Metallogeny and Mineral Assessment ; Institute of Mineral Resources ; Chinese Academy of Geological Sciences ; MLR ; Beijing 100037 ; China) ; Chen Maohong
• 刊名：Acta Geologica Sinica
• 出版年：2011
• 卷期：85(5)
• 关键词：有色金属矿 ; nonferrous metals ore ; 金矿 ; gold ores ; 银矿 ; silver ores ; 华南地区 ; South China
• 页码：p.636-658
• 图表：12 illus., 141 refs.
• 分类号：1001
• issnNo：ISSN0001-5717
• isbnNo：CN11-1951/P

uot;MARGIN: 0cm 0cm 0pt" class=MsoNormal>The Qinhang belt is located along the Qinhang (uot;urn:schemas-microsoft-com:office:smarttags" />uot;on">Qinzhou uot;on">Bay to uot;on">Hangzhou uot;on">Bay) or uot;on">Shihang uot;on">Shiwandashan Mt. to uot;on">Hangzhou uot;on">Bay) Neoproterozoic suture in uot;on">South China, which separates the Yangtze craton and Cathaysian Blocks. Based on the previous researches, the authors recognize these deposits in two episodes, i.e. Neoproterozoic marine exhalative Cu-Zn deposits, and Yanshanian granitoids related W-Sn-Cu-Pb-Zn deposits. The large-scale Late Jurassic granite related W-Sn deposits associated with the crust-source granites with input of the mantle substances at 160uot;FONT-FAMILY: 宋体; mso-ascii-font-family: ’Times New Roman’; mso-hansi-font-family: ’Times New Roman’">～150 Ma, which are inferred to be the result from subducted plate window in the central part in South China and bounded in west by the Qinhang suture, where a lot of large and supper large tin and tungsten deposits developed.