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松江河金矿区地球化异常显著。1∶5万水系沉积物测量,发育有Au、Zn、Bi、Pb等元素异常,其中Au元素异常面积16 km2,峰值24×10-9,平均值5.5×10-9,衬度10,NAP值37;1∶1万土壤测量,异常元素有Au、Ag、Cu、Sb、Pb、As等,其中Au元素异常面积达0.2178 km2,浓度分带明显,峰值253.4×10-9,平均值为29.7×10-9,异常下限3.66×10-9,平均衬度8.11,最大衬度69.23,NAP值1.767;原生晕测量,元素组合分带明显,前缘晕指示元素有Pb、As、Hg,中间成矿元素为Au、Ag、Cu,尾晕元素有W等。矿区地球化学异常特征也是重要的地球化学找矿标志。

There is significant geochemical anomaly in Songjianghe gold district.1∶50 000 stream sediment survey indicates Au,Zn,Bi,Pb anomalies and so on.And among them Au anomaly area occupies 16 km2 ,peak value is 24 × 10 -9 ,average value is 5.5 ×10 -9 ,contrast is 10,NAP value is 37;1∶10 000 soil survey shows Au,Ag,Cu,Sb,Pb,As anomalies and so on.And among them Au anomaly area occupies 0.2178 km2 ,concentration zonation is obvious,peak value is 253.4 ×10 -9 ,average value is 29.7 ×10 -9 ,bottom value is 3.66 ×10 -9 ,average contrast is 8.11,maximum contrast is 69.23,NAP is 1.767;primary halo survey suggests an obvious zonation of element association.Indication elements in front halo include Pb,As,Hg,middle mineralization elements include Au,Ag,Cu,and rear halo includes W and so on.The geochemical anomaly characteristics are also important geochemical prospecting indicators.

参考文献

[1] 吉林省地质矿产局 .中国主要成矿区(带)研究(吉林省部分)[R].长春:吉林省地质调查院,2002.
[2] 吉林省地质调查院 .吉林省敦化市松江河金矿勘探报告[R].长春:吉林省地质调查院,2012.
[3] 吉林省第五地质调查所 .金银别-白水滩水系沉积物测量报告(1:5万)[R].长春:吉林省地质调查院,1987.
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