• 责任者：Wang Yuwang (Beijing Institute of Geology for Mineral Resources ; Beijing 100012 ; China) ; Wang Jingbin
• 刊名：Geology in China
• 出版年：2012
• 卷期：39(3)
• 关键词：浅成低温热液矿床 ; epithermal deposit ; 斑岩矿床 ; porphyry deposit ; 成矿构造 ; metallotectonics
• 页码：p.695-716
• 图表：6 illus., 2 tables, 157 refs.
• 分类号：1000
• issnNo：ISSN1000-3657
• isbnNo：CN11-1167/P

The metallogenic ages of porphyry-epithermal deposits in northern Xinjiang are systemically summarized in this paper. Based on tectonic setting, the ore deposits can be classified into three types, i.e., ocean-continent subduction, collision origin composed of collision sub-type and post-collision sub-type, and intra-continent.   Porphyry deposits in different metallogenic epochs show genetic and regional “isospatial metallogenesis” characteristics and zoned distribution. From early to late the deposits expanded gradually from the position close to the suture belt outwards, and from linear distribution to planar distribution.