摘要
大青沟区铜金矿区位置处于中朝准地台,胶辽台隆、营口-宽甸台拱的东端,鸭绿江与太平哨两条北东向大断裂中间所夹持的北西向构造带中。本文通过研究区域地球化学特征,对比矿床地质特征,分析水系沉积物和土壤地球化学找矿标志,对下一步找矿工作具有重要指导意义。
The Daqinggou copper-gold mining area is located in the sino-korean paraplatform,the eastern end of Jiao-Liao platform uprise and Yingkou-Kuandian arch,in the NW trending tectonic belt between the two NE trending faults of Yalu River and Taipingshao.This paper studies the regional geochemical characteristics,compares the geological characteristics of the deposit,and analyzes the geochemical prospecting indicators of stream sediments and soil,which has important guiding significance for the next prospecting work.
作者
楚颖
CHU Ying(Liaoning Nonferrous Exploration Research Institute Co.,Ltd.,Shenyang 110013,China)
出处
《有色矿冶》
2021年第6期4-6,共3页
Non-Ferrous Mining and Metallurgy
关键词
地球化学场背景
成矿元素
地球化学异常
找矿标志
geochemical field bac kground
metallogenic elements
geochemical anomalies
prospecting sign
