摘要
笔者以地球化学原生晕理论为指导,对孟公界铀矿床1号矿体按不同标高进行了采样分析,并对分析数据进行多重数理统计;应用叠加原生晕模型对该矿床的指示性元素的轴向分带规律进行研究,建立了指示性元素自上而下的理想分带序列:Hg-As-Sb-Mo-Ag-Cu-U-W-Cd-Bi-Pb-Sr;结合不同成矿阶段的蚀变矿物组合,构建了孟公界地区热液型铀矿的矿物-蚀变-元素组合原生叠加晕模型。以此为基础,建立了原生晕预测技术指标,用于指导找矿工作。
Guided by the theory of original geochemical halo, samples at different elevation of orebody No. 1 in Menggongjie uranium deposit was collected and chemically analyzed. Statistics of the chemical data was preformed to study the vertical zonation pattern of indicating elements with superimposition model of original halos. An ideal vertical elementary zoning sequence of uranium body was established as Hg-As-Sb-Mo-Ag-Cu-U-W-Cd-Bi-Pb-Sr from up to bottom. The combination prospecting model of min- erabalteration-original element halo was set up with the alteration mineral of different ore-forming stage, which was used to constitute the geochemical forecasting technology of original halos so as to instruct the uranium exploration.
出处
《铀矿地质》
CAS
CSCD
2017年第4期215-220,245,共7页
Uranium Geology
基金
中国地质调查局“广西苗儿山地区铀矿资源调查评价”项目(编号:DD2016013611)与核能开发“桂北地区铀矿深部定位预测技术研究”项目联合资助
关键词
孟公界铀矿床
原生叠加晕
指示性元素
轴向分带
预测指标
Menggongjie uranium deposit
superimposed original geochemical halo
indicating elements
vertical zonation
forecast indictor