地质找矿论丛2011，Vol.26Issue(4)：446-452,7.
刚果(金)DIMMA铜钴矿床地质特征及成因分析
Characteristtics of Dimma Cu-Co deposit in Congo-Kinshasa and analysis on its genesis
刘运纪 1王纪昆 1张泰1
作者信息
- 1. 天津华北地质勘查总院,天津 300171
- 折叠
摘要
Abstract
Dimma Cu-Co deposit is located in the northwest end of Cu-Co ore belt in Luffilian fold arc at boundary between Congo(Kinshasa) and Zambia. It is related to volcanism and syn-sedimentary faulting and reworked by folding ,fracturing, metamorphism and secondary enrichment in late orogenic process. . Therefore, it is a polygenous Cu-Co deposit controlled by multi-factors.关键词
DIMMA铜钴矿/矿床特征/成矿流体/层控矿床/卢菲利褶皱带/刚果(金)Key words
Dimma Cu-Co deposit/characteristics of Dimma Cu-Co deposit/ore fluid/stratobound ore deposit/ Luffilian fold belt/Congo-Kinshasa分类
天文与地球科学引用本文复制引用
刘运纪,王纪昆,张泰..刚果(金)DIMMA铜钴矿床地质特征及成因分析[J].地质找矿论丛,2011,26(4):446-452,7.
