• 责任者：Lin Xi (Institute of Geology Survey and Research ; Fuzhou 350013 ; China)
• 刊名：Geology of Fujian
• 出版年：2011
• 卷期：30(2)
• 关键词：铁矿 ; iron ores ; 福建 ; Fujian Province
• 页码：p.101-107
• 图表：3 illus., 3 refs.
• 分类号：1001
• 出版序号：964
• issnNo：ISSN1001-3970
• isbnNo：CN35-1080/P

///The ore bodies of the Qingshan iron are stratiform and occur in the Late Paleozoic Jingshe formation, and form and occurrence are evidently controlled by the layer. The secondary orebody mostly acts like a veiny and lenticular. It is remarkably transformated the postmagmatic hydrothermal superimposed. It belongs to the deposit of the sedimentary-hydrothermal reforming type.