摘要
本文根据新桥铁帽型金(银)矿床地球化学资料,运用统计方法研究了矿床氧化剖面元素分带特征。通过元素间统计关系和氧化带地质地球化学信息的综合分析,认为淋积亚带中金(银)成矿,是氧化带不断氧化、分解,金、银元素不断迁移、富集的结果。
Based on statistical analysis of the geochemical data, element zoning characteristics of the Xingquiao gasson-type gold deposid is studied in this paper. A comprehensive analysis has been made of the statistical relation between elements and the geologic geochemical in formation. It is considered that gold (silver) mineralazation in sub-zone of leaching enrichbment results from the continuous oxygenolysis of the oxidzed zone, and the continuous transportand enrichment of Au and Ag.
出处
《物探化探计算技术》
CAS
CSCD
1991年第3期229-235,共7页
Computing Techniques For Geophysical and Geochemical Exploration
