摘要
Abstract
The Chelunxigou-shanggaqiang copper polymetallic deposit is located in the Cali Tōgane,copper,lead,zinc,chromium,iron and tungsten metallogenic belt,North Qilian fold belt,lenglongling complex anticline,the host rock is quartz porphyry and sand-bearing dolomite limestone of Ordovician Cherungou Group.The shape of ore body is controlled by secondary faults,fold dip end and fracture zone on both sides of the faults.关键词
甘肃省天祝县/铜多金属矿/地质特征/成矿条件Key words
Tianzhu County,Gansu Province/copper polymetallic deposit/geological characteristics/metallogenic conditions分类
天文与地球科学
