摘要
窑洞昭铜矿位于北山的北部,哈萨克斯坦板块与塔里木-北山板块的缝合部位,矿体赋存于断裂破碎带石英脉群中,为岩浆热液型矿床。大断裂两侧及次级断裂与构造破碎带中石英脉发育地带、小构造交汇部位,在硅化等蚀变发育地带、孔雀石及蓝铜矿等是区内重要的找矿标志。
The Yaodongzhao copper mine located at Beishan Mountains" north, the Kazakhstan tectonic plate and the Tal- imu-Beishan Mountains tectonic plate sutures the spot, the ore body tax saves in the break crushed zone quartz vein group, for rock magma hydrothermal ore deposit. In the big break both sides and the secondary break and the structure crushed zone the quartz vein growth region, the small structure connection spot, in alteration growth regions, the green copper ore and the azurite and so on is in the area the important prospecting symbol.
出处
《甘肃冶金》
2010年第2期52-54,58,共4页
Gansu Metallurgy
关键词
窑洞昭铜矿
地质特征
找矿标志
Yaodongzhao copper mine
geological feature
prospecting symbolized