• 责任者：Li Fushun (No.418 Geological Party ; Hunan Bureau of Geology and Mineral Resources Development ; Loudi 417000 ; China) ; Kang Ruhua
• 刊名：Geology in China
• 出版年：2012
• 卷期：39(2)
• 关键词：钨矿 ; tungsten ores ; 南岭 ; Nanling Mountains
• 页码：p.445-457
• 图表：6 illus., 5 tables, 10 refs.
• 分类号：1001
• issnNo：ISSN1000-3657
• isbnNo：CN11-1167/P

The Weijia tungsten deposit is another large-size tungsten deposit discovered recently during the new round of prospective survey for mineral resources on the northern margin of the Nanling Mountains. Based on a discussion on the metallogenic geological background, the authors studied the geological characteristics of the ore deposit. The spatial distribution of the ore body is controlled by the basement structure, lithologic character, Xianglinpu anticline, Xianglinpu granite porphyry and the concealed rock body resulting from the NE-trending intrusion of the Tongshanling granite porphyry. The secondary emplacement of the magma caused the secondary mineralization. The ore deposit is of porphyry-skarn type.