line-level: 2" class=MsoNormal>Geochemical Anomaly Characteristics of the Zhongxingtun Copper-Polymetal Deposit in Inner Mongolia

• 责任者：Li Wei (Shenyang Institute of Geology and Mineral Resources ; Shenyang 110034 ; China) ; Bi Zhongwei
• 刊名：Geology and Resources
• 出版年：2010
• 卷期：19(3)
• 关键词：铜矿 ; copper ores ; 多金属矿 ; polymetallic ores ; 地球化学异常 ; geochemical anomaly ; 内蒙古 ; Inner Mongolia
• 页码：p.267-270
• 图表：1 illus., 2 tables, 4 refs.
• 分类号：1001
• issnNo：ISSN1671-1947
• isbnNo：CN21-1458/P

The Zhongxingtun copper-polymetal deposit, located in the outer contacting belt between the epimetamorphic rocks of Paleozoic Niqiuhe formation of and the Early Jurassic fine-grained granodiorite, is of typical skarn-type. Stream sediment anomaly survey in 1∶50 000 scale and soil geochemical survey in 1∶10 000 scale show that the anomalies are mainly assemblage of Cu, Au, Ag and Bi, accompanied with W anomaly. Analysis on the geochemistry characteristics of Zhongxingtun Cu-polymetallic deposit reveals a great potential for the searching of ores of the same type in the area.