摘要
本文探讨了桦树沟铜矿床地球化学异常特征及成矿环境地球化学演化与成矿的关系，建立了桦树沟铜矿床的找矿标志。原、次生地球化学异常特征的对比表明本区次生异常与原生异常具有同样的找矿意义。
Characteristics of geological anomaly,metallogenic environment and relationship of geochemical evolution to mineralization of the Huashugou copper deposit are approached. In addition, the ore guides have been established. The comparison of the primary geochemical anomaly to the seconary one indicates that both of them have the same significance for the ore prospecting.
出处
《矿产勘查》
1995年第1期52-56,共5页
Mineral Exploration
