• 责任者：Dai Yucai (No.6 Geological Party ; Xinjiang Bureau of Geology and Mineral Resources ; Hami 839000 ; China) ; Zeng Huadong
• 刊名：Xinjiang Geology
• 出版年：2013
• 卷期：31(2)
• 关键词：硫化物矿床 ; sulfide deposit ; 新疆 ; Xinjiang
• 页码：p.161-167
• 图表：6 illus., 1 table, 4 refs.
• 分类号：1001
• issnNo：ISSN1000-8845
• isbnNo：CN65-1092/P

     The ore-bearing rocks of Poyi magmatic sulfide deposit are mainly the dunite, pyroxene peridotite, olivine pyroxenite, pyroxenite of the second period of the first intrusive mid-Variscan. The nickel orebody mainly distributed in the middle and the bottom of the ultrabasic rocks. Ore types consist of scattered disseminated, followed by sparse disseminated, a little of dense disseminated and sideronitic, semimassive-massive, vein-like. The genesis has been preliminary discussed after the analysis on the characteristic of petrography, petrochemistry, REE and trace element and mineralization of the Poyi magmatic sulfide deposit.