• 责任者：Hu Haizhu (Henan Institute of Nonferrous Metal Exploration ; Zhengzhou 450052 ; China) ; Li Nuo
• 刊名：Geology in China
• 出版年：2013
• 卷期：40(2)
• 关键词：钼矿 ; molybdenum ores ; 秦岭 ; Qinling Mountains
• 页码：p.549-565
• 图表：11 illus., 50 refs.
• 分类号：1001
• issnNo：ISSN1000-3657
• isbnNo：CN11-1167/P

     Three types of Indosinian Mo mineralization can be observed in the Qinling area, namely carbonatite-type, fault-controlled quartz vein type and porphyry type. Carbonatite-type Mo deposits are represented by the Huanglongpu and Huangshuian deposits. They are spatially and genetically associated with magmatic carbonatite, and the ore bodies are present as Mo-bearing carbonatite veins, with specific Mo+U+REE mineralization. Fault-controlled quartz vein type Mo deposits are represented by the Waifangshan Mo ore district(composed of Zhifang and Qianfanling Mo deposits), Dahu Au-Mo deposits and Majiawa Au-Mo deposits. Emphasis should be placed on Indosinian granite and related Mo mineralization in East Qinling area.