Nickel Ore Deposit Characteristic and Origin Discussion in Tiebanjing Area of Ayouqi County, Inner Mongolia
详细信息
- 责任者：Xie Chenglian （Shandong Zhengyuan Geo-Exploration Institute of CEEB ; Jinan 250014 ; China） ; Liu lei
- 刊名：Geology and Prospecting
- 出版年：2008
- 卷期：44(6)
- 关键词：镍矿 ; nickel ores ; 内蒙古
- 页码：p.27-30
- 图表：2 illus., 1 table, 1 ref.
- 分类号：1001
- issnNo：ISSN0495-5331
- isbnNo：CN11-2043/P
摘要
In Tiebanjing area, nickel ore deposits which are wholly mineralized saves in the Pyroxene-Pendotite body. This paper describes three kinds of different mineralizing processes of the formation of the rock body and nickel ore body: the gravity separation process of deep liquid state magma, the process of deep magma melting away and penetrating, the formation of rock body and nickel ore body. Based on the analyses of the three kinds of different mineralizing processes, the author concludes that, from the result of postmagmatic hydrothermal superimposition process, the whole mineralization course is a process of typical magma ore deposit formation due to the process of magma melting away.