首页|北祁连拉排沟钨矿成矿地质条件及成因分析

北祁连拉排沟钨矿成矿地质条件及成因分析

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矿区地处北祁连沟弧盆系,受区域构造影响,褶皱、断裂、地层展布均为北西向.通过对矿区成矿地质条件、异常特征、矿体特征等方面的研究,发现拉排沟钨矿床位于北祁连造山运动带内,构造地质条件复杂,其中,北大河群下岩组石英片岩为主要含矿岩性.矿区内发现钨矿体3条,钨矿化体1条,钨矿长85m~200m,厚4.14m~13.57m,W2O3品位0.11~0.39×10-2.此外,矿床成因与火山喷发活动密切相关,属(火山)沉积-变质型钨矿床.
Geological conditions and genetic analysis of the ore formation of the Labaigou Iron mine in North Qilian
The mining area is located in the North Qilian gully arc Basin system,affected by regional structure,the folds,faults and strata distribution are NW.Based on the study of ore-forming geological conditions,abnormal characteristics and orebody characteristics,it is found that the Lapaogou tungsten deposit is located in the North Qilian orogenic belt with complex structural geological conditions.Three tungsten ore bodies and one tungsten mineralized body were found in the mining area.The tungsten ore is 85m~200m long,4.14m~13.57m thick,and W2O3 grade is 0.11~0.39×10-2.In addition,the genesis of the deposit is closely related to volcanic eruption activities,and it belongs to(volcanic)sedimentation-metamorphic tungsten deposit.

North QilianPull-drain iron ore mineGeological conditionsGenesis of deposit

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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 730000

北祁连 拉排沟钨矿 地质条件 矿床成因

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.(8)