摘要
金渠金矿 842号脉位于东径 1 1 0°33′37.6″～ 1 1 0°34′1 3.6″ ,北纬 34°2 5′5 7″;厚度一般为0 .5～ 1 .0米 ;由含金石英脉及构造蚀变岩组成 ;金含量为 4.1 3% ,以自然金为主 ,银金、碲金银矿为辅 .通过对其成矿机理的分析 ,认为下一步的勘测方向应向西南进行探底 。
Jinqu gold mine vein 842 is situated at longitude 110°33'37.6'~110°34'13.6' east, latitude 34°25'57' north. The regular sickness is 0.5～1.0m. The vein is formed from quartzite and metamorphous rock. The gold content is 4.13%, containing natural gold, the most, together with argent gold and calaverite. According to the analysis of the vein formation, the next direction of prospecting should be southwest, to the edge for finding out the reserves.
出处
《洛阳师范学院学报》
2002年第2期143-145,共3页
Journal of Luoyang Normal University
关键词
金渠金矿
成矿机理
勘测
Jinqu gold mine
formation
prospecting
