构造原生晕在攻深找盲中的应用——以赣南银坑牛形坝铅锌金银矿床为例

陈伟, 谭友, 曹正端, 廖志权, 张宁发, 傅海晖

Application of tectonic primary halos in the exploration of deep concealed ore bodies: A case study of the Niuxingba plumbum-zinc-gold-silver deposit in Yinkeng, southern Jiangxi

CHEN Wei, TAN You, CAO Zheng-Duan, LIAO Zhi-Quan, ZHANG Ning-Fa, FU Hai-Hui

图4 牛形坝矿区V31号矿带(体)308号勘探线轴(垂)向原生晕元素浓度分带 1—青白口系上统库里组;2—燕山早期花岗斑岩;3—断裂构造;4—矿体及编号;5—坑道中段及标高;6—钻孔编号及孔深;7—采样点位置

Fig.4 Zonation diagram of axial(vertical)primary halo element concentration in exploration line 308 of V31 orebody in Niuxingba deposit 1—upper Qingbaikou system Kuli formation;2—early Yanshanian granitic porphyry;3—fault structure;4—ore body and number;5—middle section and elevation of gallery;6—borehole number and hole depth;7—sampling point position