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云南元阳马鹿塘金矿区地球物理、地球化学特征及找矿方向

Geophysical and geochemical characteristics and prospecting direction of Malutang Gold District in Yuanyang,Yunnan

  • 摘要: 马鹿塘金矿床位于西南三江成矿带哀牢山金成矿带南段,成矿地质条件较为有利。为实现找矿突破,对马鹿塘金矿区进行了地球物理及地球化学勘查。结果表明:矿化蚀变辉绿岩极化率最高,电阻率相对较低,具有低阻高极化特征,与围岩具有明显的电性差异,因此利用激发极化法可以圈出隐伏矿化蚀变辉绿岩及硫化物矿(化)体,激电中梯剖面测量异常显示深部仍具有较好的找矿前景;Au与As、Sb呈正相关,Au-As-Sb组合异常可作为矿区的找矿标志。物化探组合异常区及辉绿岩与围岩的接触带附近具有良好的找矿潜力,可作为进一步找矿方向。

     

    Abstract: MalutangGold Deposit is located in the south part of Ailaoshan gold metallogenic belt of Sanjiang metallogenic belt in Southwest China.Its metallogenic geological conditions are relatively favorable.In order to achieve a breakthrough in prospecting,the geophysical and geochemical exploration of Malutang Gold Deposit was carried out.The results show that the polarization rate of mineralized and altered diabase is the highest,the resistivity is relatively low,indicating the characteristics of low resistivity and high polarization and obvious electrical difference from the surrounding rock.Therefore,the scope of concealed altered mineralized diabase and sulfide ore body in this area can be delineated by induced polarization method.The abnormal measurement of IP intermediate gradient profile shows that the deep part still has a good prospecting prospect.Au is positively correlated with As and Sb,and the Au-As-Sb anomaly can be used as a prospecting indicator for gold districts.There are good potentials in combined geophysical and geochemical anomalies area and on the contact zone of diabase and surrounding rocks,which can be regarded as the next prospecting direction.

     

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