• 责任者：Zhang Zhenguo (Fujian Institute of Geology Survey and Research ; Fuzhou 350013 ; China)
• 刊名：Geology of Fujian
• 出版年：2011
• 卷期：30(3)
• 关键词：钼矿 ; molybdenum ores ; 福建 ; Fujian Province
• 页码：p.211-217
• 图表：2 illus., 3 refs.
• 分类号：1001
• 出版序号：564
• issnNo：ISSN1001-3970
• isbnNo：CN35-1080/P

The Jinghou molybdenum deposit in Jianyang City is situated at the east fringe of Northwestern Fujian mole track, in the middle of the Pucheng-Yongtai north-south-trend fault zone. It was formed in late Yenshanian, and controlled by blind porphyry body, which was controlled by Pucheng-Yongtai north-south-trend fault zone. There are three typical types of ore: line-vein Type, veinlet type, quartz vein type: quartz vein type and structurally altered rock type. The wall-rock lithology was metamorphic of the Daling Formation of Mamianshan Group in Mid-Proterozoic and adamellite in Caledonian epoch.