摘要
灵雀山金矿虽为分布在变质岩区的石英脉型金矿床,但基于控矿构造类型、低序次构造成矿特征、控矿构造与脉岩岩浆活动关系、控矿构造最佳部位的确定等,表明灵雀山金矿床主要受NNE、NW和近EW向脆性构造控制,属中生代构造-岩浆-成矿作用的产物,与区域地壳演化相一致。
Although Lingqueshan gold deposit is quartz vein type gold mine located in a large area of metamorphic rocks, but the ore-controlling structures, the subordinate structure metallogenic characters, the relationship between ore-controlling structures and magmatic activity and the determination of best ore-controlling position reveal that the deposit is mainly controlled by NNE,NW and near-EW ductile structures and is a Mesozoic production of structuremagmata-metallogenic activity, consistent with the crustal evolution in this district
出处
《黄金》
CAS
北大核心
2007年第3期11-14,共4页
Gold
关键词
控矿构造
演化模式
灵雀山金矿
山东招远
ore-controlling structure
evolutionary pattern
Lingqueshan gold deposit
