摘要
河南桐柏破山银矿床属层控中低温热液型。本文从区域、矿区、矿床地球化学特征及异常模式研究入手,总结出本类银矿床的最佳指示元素,建立了矿致异常元素的垂向和水平分带序列,对寻找该类型矿床有一定指导意义。
The deposit we studied is of the stratabound meso-epithermal type.On the basis of the features and pattern of geochamicalanomalies over this area,mining district and deposits,we have ascertaihed the optimal indicator elements and established the verti-cal and horizontal zoning sepuences of the elemients causing the occurence of ores.No doubt,this infrmation is of great importanceto the exploration of such tpye deposits.
出处
《地质与勘探》
CAS
CSCD
北大核心
1993年第6期43-48,共6页
Geology and Exploration
