摘要
甘蔗沟铅锌矿位于西成铅锌矿田中段南带,区内出露地层主要为中泥盆统安家岔组厂坝层上部层,安家岔组厂坝层上部层是西成地区重要的含矿层位,区内断裂构造发育,矿体明显受地层层位和断层双重控制,该区成矿条件良好,矿床深部具有较好的找矿空间,是寻找沉积-改造型铅锌矿床的有利地段。
Middle south zone, the main outdoor layer in the devonian series settle bifurcation set factory in dam, the upper layer, is the west into areas important ore-bearing bed, fracture structure, ore body significantly affected by stratigraphic and fault joint control, good metallogenic conditions, ore body deep has good prospecting space.It is a favorable area for searching the sedimentary-reconstructed type of lead-zinc deposit.
作者
李爱平
LI Ai-ping(Lanzhou Mineral Exploration , Gansu Nonferrous Metals Geological Exploration Bureau , Lanzhou 730046, China)
出处
《甘肃冶金》
2019年第2期63-66,71,共5页
Gansu Metallurgy
关键词
甘蔗沟铅锌矿
地质特征
双重控制
找矿前景
Ganzegou
lead-zinc ore
geological feature
double control
find-prospect