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.
引文
[1]李建中,高兆奎.西秦岭中泥盆世沉积环境及其与铅锌矿的关系[J].地质论评,1993,39(02).
[2]祝新友,汪东波,卫治国,等.甘肃西成地区南北铅锌矿带矿床成矿特征及相互关系[J].中国地质,2006,33(06).
[3]邓海军,朱多录.甘肃西成矿集区成矿系列及找矿前景[J].地质与勘探,2010,46(06).