Study on Geological Feature and Origin of Yemaquan Fe-Cu Deposit in Qimantage Area, Eastern Kunlun
详细信息
- 责任者：Song Zhongbao (Xi’an Institute of Geology and Mineral Resources ; Xi’an 710054 ; China) ; Jia Qunzi
- 刊名：Northwestern Geology
- 出版年：2010
- 卷期：43(4)
- 关键词：铁矿 ; iron ores ; 铜矿 ; copper ores ; 昆仑山 ; Kunlun Mountains
- 页码：p.209-217
- 图表：4 illus., 16 refs.
- 分类号：1001
- issnNo：ISSN1009-6248
- isbnNo：CN61-1149/P
摘要
The genesis of Yemaquan iron-polymetallic deposit was defined as skarn-type. The authors found appearance of exhalative rock and jasper rock on the top of ore deposit which give evidence to exhalative-sedimentary mineralization. By analysis of comparison, the authors considered that there is exhalative-sedimentary mineralization on the early stage, and on the later stage is skarn-type mineralization, so the origin of Yemaquan Fe-Cu deposit should be exhalative-sedimentary and skarn-type. This may have some importance in theory on prospect in Qimantage region.