地球物理勘探在青海铁多金属矿勘查中的应用  

Application of Geophysical Exploration in Exploration of Qinghai Iron Polymetallic Mine

作　　者：胡海峰 马成兴 乔世科 张胜 HU Hai-feng;MA Cheng-xing;QIAO Shi-ke;ZHANG Sheng(Qinghai Third Geological Exploration Institute,Xining 810000,China)

机构地区：[1]青海省第三地质勘查院

出　　处：《世界有色金属》2019年第16期199-201,共3页World Nonferrous Metals

摘　　要：通过对该铁多金属矿矿区控矿构造激电扫面圈定了地下矿化体的分布范围和位置,并用激电中梯确定了矿化体的埋深和产状。经过初步地质工程验证,物探推断结果与实际矿化体位置吻合较好,物探方法在该铁多金属矿找矿中取得了较好的效果。The distribution range and location of underground mineralized bodies are delineated by IP scanning of orecontrolling structures in this iron-polymetallic mine area,and the burial depth and occurrence of mineralized bodies are determined by IP intermediate elevator.After preliminary geological engineering verification,the geophysical inference results are in good agreement with the actual mineralization position,and the geophysical prospecting method has achieved good results in the iron polymetallic ore prospecting.

关 键 词：铁多金属矿 激电扫面 激电中梯 矿化体 

分 类 号：P618.2[天文地球—矿床学] P631[天文地球—地质学]