地球化学定量预测法在区域矿产调查中的应用——以新疆比勒提地区为例
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张辉, 马庆, 宋贺民, 王占彬, 王兵, 牛学瑶
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The application of geochemical quantitative prediction methods to regional geological and mineral survey:A case study of Beliti area,Xinjiang
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Hui ZHANG, Qing MA, He-Min SONG, Zhan-Bin WANG, Bing WANG, Xue-Yao NIU
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表3 喀拉铁克金铜铅锌成矿远景区Hs-4号异常部分单元素异常参数
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| 异常编号 | 异常点数 | 异常面积/km2 | 极大值 | 平均值 | 标准离差 | 衬度值 | 规模 | 浓度分带 | | Hs-Au16 | 11 | 1.42 | 5.00 | 3.35 | 0.68 | 1.34 | 1.21 | 2 | | Hs-Au15 | 43 | 7.10 | 22.10 | 4.71 | 3.36 | 1.88 | 15.68 | 3 | | Hs-Cu4 | 6 | 0.73 | 48.80 | 44.92 | 2.95 | 1.12 | 3.59 | 1 | | Hs-Cu6 | 4 | 0.43 | 54.90 | 49.63 | 5.68 | 1.24 | 4.17 | 1 | | Hs-Ni11 | 63 | 11.94 | 228.00 | 50.16 | 24.47 | 1.25 | 121.29 | 3 | | Hs-B10 | 49 | 9.63 | 78.00 | 64.83 | 5.82 | 1.18 | 94.64 | 1 | | Hs-As5 | 49 | 8.41 | 42.30 | 23.60 | 6.00 | 1.31 | 47.12 | 2 | | Hs-Zn11 | 47 | 8.67 | 115.00 | 98.18 | 5.55 | 1.09 | 70.93 | 1 | | Hs-V7 | 46 | 8.09 | 162.00 | 121.02 | 10.18 | 1.10 | 89.19 | 1 | | Hs-Bi11 | 49 | 7.75 | 0.69 | 0.45 | 0.05 | 1.13 | 0.40 | 1 | | Hs-Cr6 | 34 | 5.98 | 466.00 | 114.18 | 64.59 | 1.27 | 144.62 | 3 | | Hs-W8 | 32 | 5.61 | 3.60 | 2.66 | 0.29 | 1.21 | 2.58 | 1 | | Hs-Sb14 | 31 | 5.37 | 1.84 | 1.33 | 0.17 | 1.21 | 1.22 | 1 | | Hs-Ni17 | 25 | 5.04 | 50.20 | 43.29 | 2.81 | 1.08 | 16.58 | 1 | | Hs-Zn17 | 24 | 4.53 | 133.00 | 98.88 | 9.17 | 1.10 | 40.20 | 1 | | Hs-Sb16 | 28 | 3.97 | 1.61 | 1.24 | 0.11 | 1.13 | 0.55 | 1 | | Hs-Sn12 | 16 | 1.94 | 4.30 | 3.84 | 0.26 | 1.10 | 0.67 | 1 | | Hs-Sn13 | 8 | 1.93 | 4.50 | 3.83 | 0.32 | 1.09 | 0.63 | 1 |
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