摘要
对湖南龙山金锑矿中微量元素进行参数统计显示,Au、Ag、As、Sb、W、Cu元素含量相对高,变化系数较大,易形成实质性的地球化学异常;因子分析、聚类分析表明,Au、As、Sb、Cu元素代表主要成矿元素的组合;对应分析表明,蚀变板岩的形成与Au的成矿热液活动关系较密切;元素分布型式显示,Au、As、Sb元素代表了主要成矿元素的富集组合,其分布范围广,离散度大,可作为本区找矿的指示元素。
The statistics of trace element parameters show that the contents of Au,Ag,As,Sb,W,Cu are relatively high,the coefficient of variation is large,and it is easy to form substantial geochemical anomalies.Factor analysis and cluster analysis show that au,Ag,As,Sb and Cu represent the assemblage of the main ore-forming elements,and the corresponding analysis shows that the formation of altered slate is closely related to the ore-forming hydrothermal activity of au.The distribution patterns and fractal statistical characteristics of elements show that Au,As and Sb elements represent the enrichment and assemblage of the main ore-forming elements,which can be used as indicator elements for prospecting in this area because of their wide distribution range and large dispersion.
作者
黄一杰
苏特
HUANG Yi-jie;SU Te(Geology Team NO.4 of Guangxi Zhuang Autonomic Region,Nanning 530000,China;College of Earth Science,Guilin University of Technology,Guilin 541004,China)
出处
《世界有色金属》
2020年第11期155-155,共1页
World Nonferrous Metals
关键词
岩石地球化学
金锑矿
龙山
湖南
rock geochemistry
gold antimony deposit
Longshan
Hunan