• 责任者：Liu Feng (Key Laboratory of Metallogeny and Mineral Assessment ; Institute of Mineral Resources ; Chinese Academy of Geological Sciences ; Beijing 100037 ; China) ; Yang Fuquan
• 刊名：Mineral Deposits
• 出版年：2009
• 卷期：28(3)
• 关键词：铁矿 ; iron ores ; 新疆 ; Xinjiang
• 页码：p.251-264
• 图表：5 illus., 3 tables, 43 refs.
• 分类号：1001
• issnNo：ISSN0258-7106
• isbnNo：CN11-1965/P

Located in Late Silurian-Early Devonian felsic volcanic rocks along the southern margin of Altay, the Abagong iron deposit occurs as lens, veins and stratoid bodies controlled by volcanic fault structures, with an obvious boundary between the iron body and the host rocks, unclear alteration in host rocks, high ore grade and coexisting apatite and magnetite in iron ore. These features suggest that the Abagong iron deposit is comparable with the Kiruna type iron deposit in northern Sweden and the porphyrite iron deposits in Ningwu area. The characteristics indicate that the Abagong iron ore deposit, the Kiruna type iron ore deposit in northern Sweden and the porphyrite iron ore deposits in Ningwu area have a common genesis of magmatic differentiation.