【摘要】 以重庆市小茶园锰矿为研究对象,详细叙述了锰矿床地质特征。研究表明,该矿床形成受古构造、岩相对锰矿的控制,小茶园矿集区主要位于楠木庄断层与青华断层共同控制的局限成锰槽盆之中,岩相组合特征指示矿床位于过渡相和中心相。更多还原

【Abstract】 The paper takes Xiaochayuan Manganese Ore in Chongqing as research object,describing the manganese ore deposit geological characteristics in detail.The study shows that the formation of this ore deposit is under the control of paleostructure and lithofacies on manganese ore.Xiaochayuan ore concentrated area is mainly located in the limited manganese trough basin controlled by Nanmuzhuang fault and Qinghua fault.The characteristics of lithofacies combination indicate that the ore deposit is in transient phase and central phase.更多还原