摘要
小柳沟北铁铅锌多金属矿位于柳沟峡-九个青羊元古宙、加里东期铜铁金铅锌钨(铬)Ⅳ级成矿带上,总结了该区地层、构造、岩浆岩、变质作用等成矿条件与多金属矿的关系,初步认为矿体成因属中低温热液变质岩型多金属矿床。
Xiaoliugou north iron lead zinc polymetallic ore deposit is located in the liugouxia-nine blue sheep proterozoic-caledonian periodcopper-iron-gold-lead-zinc-tungsten(chromium) grade Ⅳ Metallogenic belt,The relationship between metallogenic conditions such as strata,structure,magmatic rock and polymetallic ore is summarized,The genesis of the ore body is believed to be a polymetallic deposit of medium and low temperature hydrothermal metamorphic rock type.
引文
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