• 责任者：Hao Junjie (No.11 Geological Party ; Hebei Exploration Bureau of Geology and Mineral Resources ; Xingtai 054000 ; China) ; Xin Jianhong
• 刊名：Geoscience
• 出版年：2011
• 卷期：25(3)
• 关键词：铁矿 ; iron ores ; 稀土元素 ; rare earths ; 河北 ; Hebei Province
• 页码：p.545-552
• 图表：6 illus., 3 tables, 23 refs.
• 分类号：1001
• issnNo：ISSN1000-8527
• isbnNo：CN11-2035/P

Based on the study of REE geochemistry of Baijian iron deposit in Shahe, Hebei Province, REE in skarns, ores and strata limestone have the similar characteristics, and ores are closely related to magmatic rocks (diorites). REE pattern of ores show the same distribution pattern of limestones of wallrocks. A probable reason of the phenomenon is inferred that ore-forming fluids or magma experienced long distance transportation after forming, went through structures such as faults to the deposition place, and then acted metasomatism with wallrocks, and that during metasomatism, ore-forming fluids extracted ore-forming materials from wallrocks.