铜钼矿床的地质特征及找矿潜力分析

Geological characteristics and prospecting potential of copper molybdenum deposits

铜钼矿床有夕卡岩型和斑岩型两类矿化,是鄂东南矿集区内典型的夕卡岩斑岩复合型矿床。本文以大黑山矿区为例,介绍了大黑山矿区的的山势走向,山体主要组成成分并对矿区的元素含量进行了分析,有两个断层,分别是F1、F2,通过对坡度的分析进一步探求了断层的构造。根据初步分析,确定铜钼矿床的形成与地层、构造、风力作用有着直接的关系,是一种经过时间的沉积不断增加的矿床。在大黑山的东面和北部矿资源丰富,为后期寻找铜钼矿床建立了矿点以及后期的勘察工作更加方便进行。

There are two types of mineralization in Cu Mo deposit,skarn type and porphyry type.It is a typical skarn porphyry compound deposit in the ore concentration area of Southeast Hubei.Taking Daheishan mining area as an example,this paper introduces the mountain trend,the main components of the mountain and the element content of Daheishan mining area.There are two faults,F1 and F2.Through the analysis of the slope,the structure of the fault is further explored.According to the preliminary analysis,it is determined that the formation of the copper molybdenum deposit is directly related to the strata,structure and wind force,and it is a deposit with increasing deposition over time.There are abundant mineral resources in the East and north of Daheishan,which makes it more convenient to search for copper and molybdenum deposits in the later period and to carry out the exploration work in the later period.