摘要
文章对博茨瓦纳铜镍硫化物矿床的研究成果进行了总结,概括了赛莱比-皮奎铜镍硫化物矿床的区域地质背景、岩石地层划分,较系统地分析了矿床的地质特征和矿床成因;认为铜镍硫化物矿床的成矿物质来源多样,并且矿床形成后经历了强烈的褶皱和剪切作用。
The paper summarizes result of the previous researches on Cu-Ni deposits in Botswana inclu- ding the regional geological background of Selebi-Phikwe Cu-Ni deposit, stratigraphic division, systematic analysis of geological characteristics and genesis of the deposit. The authors think that ore material of the deposit is derived from multi-sources and it is exposed to strong post-ore folding and shearing.
出处
《地质找矿论丛》
CAS
CSCD
2015年第A01期129-136,共8页
Contributions to Geology and Mineral Resources Research
基金
中国地质调查局项目<非洲中南部重要矿床地质背景
成矿作用和找矿潜力研究>(编号:1212011220910)
国外风险勘查基金项目(编号:科[2011]D3-04)资助
