首页|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

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

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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.
Geological characteristics and metallogenic conditions of the Chelunxigou-shanggaqiang copper polymetallic deposit in Tianzhu County,Gansu province
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.

Tianzhu County,Gansu Provincecopper polymetallic depositgeological characteristicsmetallogenic conditions

李永和

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甘肃省有色金属地质勘查局兰州矿产勘查院,甘肃 兰州 730030

甘肃省天祝县 铜多金属矿 地质特征 成矿条件

2024

世界有色金属
有色金属技术经济研究院

世界有色金属

影响因子:0.138
ISSN:1002-5065
年,卷(期):2024.(11)