摘要
拉伊克勒克铁铜矿床位于唐巴勒-卡拉麦里古生代复合沟弧带内,容矿地层为早泥盆世托让格库都克组一套火山岩地层,赋矿岩石主要为矽卡岩,主要矿体呈似层状、透镜体状产出,严格受岩性控制,矿石具浸染状、块状、网环状、假斑状、斑杂状和团块状构造。通过近几年来的地质勘查及综合分析,认为拉伊克勒克铁铜矿床成因类型属矽卡岩型铁铜矿。
The Ciric Rai iron-copper deposit is located in the tangbale - Cara Mai Li composite Paleozoic trench arc zone, the host strata is a set of volcanic rock strata of early Devonian Tuoranggekuduke group, host rocks are mainly skarns, ore bodies presents stratiform, lens-shaped output, which strictly controlled by lithology, minerals have disseminated, massive, net circular, pseudoporphyritic, taxitic and cumby structure. Through the geological survey and comprehensive analysis in recent years, it is suggested that the Ciric Rai iron-copper deposit belongs to skaru type iron-copper deposit due to its genetic type.
出处
《甘肃冶金》
2017年第3期43-44,47,共3页
Gansu Metallurgy
