摘要
文中通过两期在缅甸莫苇塘镍矿区野外地质填图的实践与探索,在对镍矿区地质填图工作总结的基础上根据所获取的认识对镍矿的矿床成因进行了较深入的分析与探讨,并结合两期报告综合研究的成果,作出矿床成因类型为"原生含镍超基性岩在表生风化作用下红土化过程中形成的硅酸盐镍矿床"的结论。
By two-stage geological mapping practice and summary of nickel deposit in Myanmar Mwetanng area, according to the knowledge obtained on them and comprehensive study to the genesis of deposit in two-stage reports, the conclusion is drawn in this paper that primary nickel ultrabasic rocks form silicate nickel deposit under the process of laterite in the surface weathering.
出处
《有色金属(矿山部分)》
2009年第4期25-28,共4页
NONFERROUS METALS(Mining Section)
关键词
地质填图
矿石自然类型
矿床工业类型
垂向分带
找矿标志
红土硅酸盐镍矿床
geological mapping
ore natural type
deposit industrial type
vertical zoning
prospecting signals
lateritic silicate nickel deposit