甘肃省天祝县车轮西沟-上嘎墙一带铜多金属矿地质特征及成矿条件浅析
Geological characteristics and metallogenic conditions of the Chelunxigou-shanggaqiang copper polymetallic deposit in Tianzhu County,Gansu province
李永和1
作者信息
- 1. 甘肃省有色金属地质勘查局兰州矿产勘查院,甘肃 兰州 730030
- 折叠
摘要
车轮西沟-上嘎墙一带铜多金属矿位于北祁连加里东金、铜、铅、锌、铬、铁、钨成矿带上,北祁连褶皱带冷龙岭复背斜,赋矿岩性为奥陶系车轮沟群英安斑岩、含砂白云质灰岩,矿体形态受断裂两侧的次级断裂、褶皱倾伏端、破碎带控制.
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引用本文复制引用
出版年
2024
国家科技期刊平台
NSTL
万方数据