- 责任者：Zhao Yiming (Key Laboratory of Metallogeny and Mineral Assessment ; MLR ; Institute of Mineral Resources ; Chinese Academy of Geological Sciences ; Beijing 100037 ; China)
- 刊名：Mineral Deposits
- 出版年：2013
- 卷期：32(4)
- 关键词：铁矿 ; iron ores ; 中国 ; China
- 页码：p.686-705
- 图表：8 illus., 2 tables, 58 refs.
- 分类号：1001
- issnNo：ISSN0258-7106
- isbnNo：CN11-1965/P
The proven total reserves of iron ores in China are relatively abundant, but the iron ores mainly belong to low-grade ores. The main genetic types of iron deposits of high-grade ores in China include： 1）hydrothermal reformed type in sedimentary metamorphosed iron deposits (BIF); 2) weathered leaching type in sedimentary metamorphosed iron deposits (BIF); 3) iron deposits related to continental volcano-intrusive activities; 4) iron deposits related to marine volcanic (intrusive) activities; 5) skarn iron deposits; and 6) hydrothermal iron deposits. Among these iron deposit types of high-grade iron ores, the skarn iron deposits and iron deposits related to marine volcanic (intrusive) activities are relatively important and have favorable ore-prospecting potential.