• 责任者：Zhao Guobin (Xi’an Institute of Geology and Mineral Resources ; Xi’an 710054 ; China) ; Li Wenming
• 刊名：Geology and Prospecting
• 出版年：2011
• 卷期：47(5)
• 关键词：花岗岩 ; granite ; 地球化学 ; geochemistry ; 成因矿物学 ; genetic mineralogy ; 内蒙古 ; Inner Mongolia
• 页码：p.828-836
• 图表：4 illus., 1 table, 29 refs.
• 分类号：0803
• issnNo：ISSN0495-5331
• isbnNo：CN11-2043/P

///Located in the western Pantuoshan-Gudongjing compressional uplift zone, the Beishan Mountains in Inner Mongolia, the Pantuoshan granite body is a complex intrusion comprised of granodiorite and K-feldspar granite. In the Devonian, this region was in the plate collision orogenic stage, and power was converted into heat, which resulted in the partially re-melted pre-Cambrian ancient continental crust, and the later tungsten-bearing granitic magma. The mineralization of Pantuoshan granite bodies can be divided into two periods.