内蒙古丰镇市开花山银多金属矿矿床地质特征及成因分析

Analysis on Geological Characteristics and the Origin of Silver Polymetallic Deposit in Kaihuashan in Fengzhen Town of Inner Mongolia

摘要:

内蒙古丰镇市开花山银多金属矿床赋存于太古宙集宁（岩）群片麻岩分布区的构造破碎带中，为小型银多金属矿矿床，共揭露3个矿体，矿体规模较小，矿石结构简单，矿石品位相对较稳定。岩浆热液和断裂构造破碎带对成矿、控矿具有重要作用。矿床成因属浅成中低温热液型矿床。

Abstract:

Kaihuashan silver polymetallic deposit in Fengzhen town in Inner Mongolia occurred in fractural zones of Archean Jining group. It is a small type silver polymetallic deposit .Three ore deposits have been exposed totally with small scale, simple ore structure and stable ore grades. The magmatic hydrothermal and fault fracture zones play important roles in ore formation and control. Iris medium and low temperature magmatic hydrothermal type deposit.