SPECTRAL CHARACTERISTICS OF ALTERATION MINERALS AND ITS APPLICATION IN GOLD DEPOSIT PROSPECTING IN WULONGGOU, QINGHAI PROVINCE
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摘要: 使用近红外光谱仪对五龙沟金矿区主要蚀变矿物进行了光谱测试,获得该矿区主要蚀变矿物的光谱数据;同时选择部分具有代表性的样品进行详细的镜下鉴定,并将镜下鉴定结果与野外实测光谱曲线进行对比分析,检查其对五龙沟金矿体矿化蚀变快速检测的有效性和准确度。对比分析结果表明,蚀变分带与矿体吻合较好,对矿化分带具有较好的指示意义,也为该区的金矿勘探提供了依据。Abstract: Near-Infrared Spectrometer was used to investigate main alteration minerals in Wulonggou gold deposit and got their spectroscopic data. The typical samples were chosen for detailed microscopic identification, and the result was compared with the filed spectrometer curve. The efficiency and accuracy of gold deposit alternation fast investigation was checked. The analysis showed alteration zonation was well in accord with ore body, had a better guidance for mineralization, and supplied dependence for gold deposit exploration.
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Key words:
- spectrum curve /
- alteration mineral /
- Wulonggou gold deposit
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图 1 五龙沟金矿矿区地质简图(陆露,2011;据五龙沟金矿内部研究报告修编,2008)
1—第四系风成砂;2—第四系冲洪积砂、砾石层;3—青白口系变火山岩组;4—青白口系丘吉东沟组;5—长城系小庙组上段;6—长城系小庙组下段;7—下元古代白沙河岩组;8—泥盆纪侵入岩-淡肉红色中粗粒黑云母钾长花岗岩;9—泥盆纪侵入岩-灰-浅灰色中粗粒二长花岗岩;10—晚志留纪侵入岩;11—晚志留纪-晚泥盆纪侵入岩;12—寒武纪侵入岩-浅灰中粗粒二长花岗岩;13—寒武纪侵入岩-浅灰黑云母花岗闪长岩;14—晚元古代侵入岩-浅灰中粗粒黑云母花岗闪长岩;15—晚元古代侵入岩-灰色中细粒石英闪长岩;16—肉红色中粒强蚀变钾长花岗岩;17—深灰绿色中粒硅化角闪辉长石;18—尖黑山单元:灰绿色透闪石化橄辉岩;19—二长花岗岩脉;20—黑云母花岗岩脉;21—石英脉;22—花岗岩脉;23—钾长花岗岩脉;24—闪长岩脉;25—辉绿玢岩脉;26—辉石闪长岩脉;27—闪长玢岩脉;28—石英闪长岩脉;29—岩脉;30—岩层产状;31—岩石片理产状;32—岩石片麻理产状;33—断层;34—韧性剪切带;35—地层界线;36—背斜轴迹;37—倒装向斜轴迹;38—向斜轴迹;39—小型金矿床位置;40—中型金矿床位置;41—大型金矿床位置;42—铜金属矿化位置点;43—多金属矿化位置点;44—金矿化点;45—铁矿化位置点;46—钼矿化位置点;47—多金属矿点;48—铅锌矿点位
Figure 1. Geological sketch map of WuLonggou gold deposit
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