摘要
谢通门—南木林地区主成矿元素呈东西向展布且具清晰的分带性,与区内主构造格局基本一致;化探异常受构造和岩浆弧带控制和约束。北部区域是寻找铅锌银多金属矿的有利地带;东南地区是寻找高温热液钨钼多金属矿产及磁铁矿的有利地段;南部是铜金类矿产富集成矿的有利地带。
Generally accordant to dominant tectonic framework in this area, major metallogenic dis- tribution in the Xietongmen-Nanmuling area presents at east-west direction with clear zoning appear- ance, in which geochemical anomalies are confined in the regional tectonic framework and magma arc belts. Polymetallic ores including lead-zinc-silver mineralization are prospective in the north part of this area; high temperature hydrothermal polymetallic ores of tungsten？molybdenum and magnetite mineralization are prospective in the southeast area; and copper-gold-bearing ores mainly occur in the south area.
出处
《陕西地质》
2015年第2期34-39,共6页
Geology of Shaanxi
基金
青藏专项:中国地质调查局:西藏1:20万谢通门幅南木林县幅区域化探(1212010818005)
