高级检索

    陕西镇安杨泗钼矿地质特征及成因浅析

    Geology and metallogenic mode of the Yangsi molybdenum deposit in Zhen'an, Shaanxi

    • 摘要: 陕西镇安杨泗钼矿位于四海坪岩体北缘,赋存于古元古界陡岭岩群与四海坪岩体的外接触带。通过野外勘查、测试分析和综合研究,在研究区内共圈定4条钼矿体,矿石类型主要为石英脉型辉钼矿石;该钼矿床受构造-岩浆作用控制明显,含矿热液沿导矿构造迁移并富集成矿,为该地区进一步(分析)寻找同类钼矿提供借鉴。

       

      Abstract: Yangsi molybdenum deposit in Zhen’an, Shaanxi is located in the north edge of Sihaiping rock mass, and occurs in the outer contact zone between the Lower Proterozoic Douling rock group and Sihaiping rock mass. Through field exploration, test analysis and comprehensive research, four molybdenum ore bodies are delineated in the study area, and the ore type was mainly quartz vein molybdenum. The molybdenum deposit is obviously controlled by tectono-magmatism,and the ore-bearing hydrothermal solution has migrated and enriched along the ore-conducting structure, which provides a reference for further prospecting of the same type of molybdenum deposit in this area.

       

    /

    返回文章
    返回