白山堂铜矿—矿带地质特征及成因浅析
Gansu Science and Technology（2021）
Abstract
白山堂铜矿是甘肃北山成矿带典型的铜矿床.F1断裂为区域断裂的次级断裂,该断裂控制了次火山岩岩墙以及主要含矿层位次生石英岩的空间分布,为重要的容矿构造,通过分析F1与次火山岩岩墙、矿体的关系得出白山堂铜矿属于受构造控制的岩浆期后热液型矿床.
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