ARGIN: 0cm 0cm 0pt; mso-margin-top-alt: auto; mso-margin-bottom-alt: auto; mso-pagination: widow-orphan; mso-outline-level: 2" class=MsoNormal>ack; FONT-SIZE: 12pt; mso-bidi-font-family: 宋体; mso-font-kerning: 18.0pt" lang=EN-US>Geochemical Anomaly Characteristics of the Zhongxingtun Copper-Polymetal Deposit in amespace prefix = st1 ns = "urn:schemas-microsoft-com:office:smarttags" />
- 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
ARGIN: 0cm 0cm 0pt" class=MsoNormal>ang=EN-US>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 1amily: 宋体">∶ang=EN-US>50 000 scale and soil geochemical survey in 1amily: 宋体">∶ang=EN-US>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.amespace prefix = o ns = "urn:schemas-microsoft-com:office:office" />