line-level: 2">Geology and Genesis of the Daolundaba Copper-Polymetal Deposit in Inner Mongolia

• 责任者：Li Zhenxiang (No.10 Institute of Geological Exploration ; Inner Mongolia Bureau of Geology and Mineral Resources ; Chifeng 024005 ; China) ; Zhuo Fuhua
• 刊名：Geology and Resources
• 出版年：2009
• 卷期：18(1)
• 关键词：铜矿 ; copper ores ; 内蒙古 ; Inner Mongolia
• 页码：p.27-30
• 分类号：1001
• issnNo：ISSN1671-1947
• isbnNo：CN21-1458/P

The Daolundaba Cu-polymetal deposit in Xi Ujimqin Qi, Inner Mongolia, occurring in the structural fissures of NE-trending fault belt, is strictly controlled by the fault structure. The deposit is of filling-metasomatic vein type, genetically belonging to meso-hydrothermal deposit. The deposit is located in the Xilinhot-Huolin Gol polymetal metallogenetic belt in the middle-south of Daxinganling Mountains, with developed structure and frequent volcanic activities. The Cu-polymetallic mineralization is in multiple stages. The orebodies are in small-medium scale, with complex shapes, stable thickness, even or uneven compositions and developed wallrock alteration.