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    陕西华阴塬头碳酸岩石英脉型钼矿床地质特征及成因探讨

    Geological characteristics and genesis of carbonate quartz vein type molybdenum deposit in Huayin Yuantou, Shaanxi Province

    • 摘要: 华阴塬头Q1001厚脉型钼矿床位于金堆城-黄龙铺钼矿成矿区,区内分布太华岩群和高山组地层,区域构造复杂,岩浆活动强烈,方解石石英脉发育,钼矿床(点)分布密集。研究矿床产于太华群地层及晋宁期片麻状花岗岩中,受南北向断裂控制;是区内发现的规模较大,品位较富的钼矿床;为厚大碳酸岩石英脉型钼矿床;矿床中除钼之外伴生铅、稀土矿产。对该矿床地质特征进行全面总结和研究,将对区内脉型钼矿及铅、稀土等矿产的找矿工作具有借鉴和指导意义。

       

      Abstract: Huayin Loess Q1001 thick vein-type molybdenum deposit is located in the Jinduicheng-Huanglongpu molybdenum deposit area,where the Taihua Group and Jixian Alpine Formation are distributed,the regional tectonics are complex,the magmatic activity is strong,calcite quartz veins are developed,and molybdenum deposits are densely distributed(points).The deposit is located in Taihua formation and Jinning period gneissic granite,controlled by the northsouth fracture,which is a large scale molybdenum deposit found in the area with rich grade,and it is a thick carbonate quartz vein type molybdenum deposit,which is accompanied by lead and rare earth minerals.A comprehensive summary and study of the geological characteristics of the deposit will play a certain guiding role in the prospecting of vein type molybdenum deposits in the area.

       

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