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An analysis of multivariate uranium metallogenic information and metallogenic prognosis in Linxi-Ulanhot area |
En ZHANG1,2, Ming DUAN3, Hui-Xiong LU1,2, Bo FENG1, Qiu-Yi CAO1,2, Yan-Chao YANG1 |
1. Airborne Survey and Remote Sensing Center of Nuclear Industry, Shijiazhuang 050002,China 2. Faculty of Earth Sciences, East China Institute of Technology, Nanchang 330170,China 3. Tianjin Center of China Geological Survey, Tianjin 330017,China |
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Abstract Located in the south-central part of Da Hinggan Mountains uranium metallogenic province, Linxi-Ulanhot area is characterized by strong tectonic magmatic activity and favorable geological conditions for uranium mineralization. Limited by such factors as vegetation development and thick cover, it is difficult for the single exploration method to meet the demand of the current deep prospecting. Based on the analysis of ore-forming conditions and ore-controlling factors, the authors constructed a comprehensive volcanic-type uranium ore comprehensive prospecting model by integrating such pieces of multivariate information as airborne radioactivity, aeromagnetic survey, geochemistry and remote sensing. Using spatial analysis function of the geographic information system (GIS), the authors extracted the multivariate prospecting information, carried out quantitative prognosis for uranium ore by evidence weighting method, and selected 16 evidence layers closely related to mineralization. Among them, the Upper Jurassic Manketouebo Formation is the main ore-bearing strata, the Late Jurassic-Early Cretaceous subvolcanic rocks are closely related to ore formation, the ore-controlling effect of NE-NNE trending fracture is significant, and uranium mineralization is mostly developed in the fault-dense zone and the intersection zone. Such anomalies as airborne radioactive anomalies (U high field, F high value halo, U/K high value halo, Hu low value halo), geochemical anomalies (Mo, Ag, Pb, W, Sn) and remote sensing alterations (Iron alteration, hydroxy alteration) play important roles in the indication of volcanic uranium mineralization. According to the posterior probability determined by the evidence weight method, 18 prospective areas were delineated, covering most uranium deposits (ore spots) in the area, indicating that the prediction results are reliable. In seven of them, uranium deposits (ore spots) were found for the first time. All these places have excellent metallogenic geological conditions, rich prospecting clues and good prospecting prospects, and the results obtained by the authors have certain guiding significance for further prospecting.
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Received: 26 September 2018
Published: 25 October 2019
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矿床 (点) | 成矿 类型 | 地层 | 潜火 山岩 | 构造 方向 | 放射性 异常 | 航磁 区间 | 化探 异常 | 遥感 蚀变 | 701 矿床 | 蚀变裂 隙带型 | 满克头鄂博 组、哲斯组 | | EW | 地面伽玛 高场 | — | Mo、Ag | 铁染、羟 基异常 | 78510 矿点 | 蚀变裂 隙带型 | 玛尼吐组 | | SN、NE | 航放铀高场、 U/K高值晕 | 50~75 nT | Mo、Pb、Cu | 铁染 异常 | 25 矿点 | 潜火山 岩型 | 满克头 鄂博组 | 花岗 斑岩 | SN、NE | 航放铀高场、铀增 量及U/K高值晕 | -100~-75 nT | Mo | 铁染、羟 基异常 | 306 矿点 | 潜火山 岩型 | 白音高老组 | 流纹 斑岩 | NW、NE | 地面伽玛 高场 | — | Cu、Pb、Zn、 Mo、Sn | 羟基 异常 | 3044 矿点 | 潜火山 岩型 | 满克头 鄂博组 | 石英 斑岩 | EW、NE | 地面伽玛 高场 | — | Pb、Zn、Sn、 Mo | 羟基、铁 染异常 |
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Multi-source prospecting informations for uranium deposits in the region
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Distribution of main ore-bearing strata in Linxi-Ulanhot area 1—Baiyingaolao formation;2—Manitu formation;3—Manketou Obo formation;4—uranium deposit and uranium occurrences and uranium mineralization point;5—study area
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Distribution of faults in Linxi-Ulanhot area 1—regional fault;2—general fault;3—uranium deposit and uranium occurrences and uranium mineralized site;4—study area
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航放参数 | 数学模型 | 单位 | 地质意义 | 铀增量 | ΔU=U-U' | 10-6 | U'为同一地质单元铀含量平均值;ΔU正值晕表示铀迁入,并反映迁出量;ΔU负值晕表示铀迁出 | F | F=U×K/Th | 10-2 | 指示蚀变带,非蚀变岩比值小,蚀变岩比值大 | 铀钾比 | U/K | 10-4 | 增强显示钾、铀含量变化的局部性差异,突出显示钾钠交代作用 | 活性铀 | Hu=(Th/b)-U | 10-6 | 初始铀含量与现今铀含量之间的差值,表征成岩后铀活化迁移的数值。b为同一地质单元各测点钍/铀比值的平均值 |
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Mathematical model of airborne radioactive parameters and geological significance
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Distribution of geochemical anomalies in Linxi- Ulanhot area 1—Cu anomaly;2—Pb anomaly;3—Zn anomaly;4—Mo anomaly;5—Ag anomaly;6—W anomaly;7—Sn anomaly;8—uranium deposit and uranium occurrences and uranium mineralized site;9—study area
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地层 | 矿床规模个数 | N/个 | S/km2 | M/(个/km2) | F/% | C | 矿床 | 矿点 | 矿化点 | 白音高老组 | 0 | 0 | 8 | 8 | 10866 | 0.0007 | 5.16 | -0.944 | 玛尼吐组 | 0 | 1 | 8 | 13 | 7344 | 0.0017 | 8.39 | -0.295 | 满克头鄂博组 | 1 | 6 | 72 | 112 | 7096 | 0.0158 | 72.26 | 2.461 |
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Beneficial degree of rock formations
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缓冲半径 /km | 矿床规模个数 | N/个 | S/km2 | M/(个/km2) | F/% | C | 矿床 | 矿点 | 矿化点 | 0.5 | 0 | 2 | 19 | 29 | 7757 | 0.0037 | 18.71 | 0.827 | 1.0 | 1 | 2 | 28 | 48 | 13916 | 0.0035 | 34.97 | 0.700 | 1.5 | 1 | 3 | 42 | 67 | 20490 | 0.0032 | 43.22 | 0.852 | 2.0 | 1 | 4 | 59 | 104 | 27063 | 0.0038 | 67.10 | 1.094 | 2.5 | 1 | 5 | 62 | 110 | 33381 | 0.0033 | 70.10 | 1.037 | 3.0 | 1 | 5 | 87 | 122 | 39174 | 0.0026 | 78.71 | 1.008 |
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Beneficial degree of buffer zone of the Late Jurassic-Early Cretaceous sub-volcanic rocks
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参数 | 矿床规模个数 | N/个 | S/km2 | M/(个/km2) | F/% | C | 矿床 | 矿点 | 矿化点 | U高场 | 0 | 4 | 75 | 95 | 4024 | 0.0236 | 85.59 | 2.987 | ΔU高值晕 | 0 | 3 | 71 | 86 | 2962 | 0.0290 | 77.48 | 2.607 | F参数高值晕 | 0 | 4 | 57 | 77 | 1881 | 0.0409 | 69.37 | 2.417 | U/K高值晕 | 0 | 5 | 66 | 86 | 2723 | 0.0316 | 77.48 | 2.842 | Hu低值晕 | 0 | 3 | 69 | 84 | 3223 | 0.0261 | 75.68 | 2.619 |
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Beneficial degree of airborne radioactive characteristic parameters
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元素 | 矿床规模个数 | N/个 | S/km2 | M/(个/km2) | F/% | C | 矿床 | 矿点 | 矿化点 | Cu | 0 | 0 | 10 | 10 | 3643 | 0.0027 | 6.45 | 0.824 | Pb | 0 | 3 | 32 | 47 | 7975 | 0.0059 | 30.32 | 1.667 | Zn | 0 | 3 | 16 | 31 | 8912 | 0.0035 | 20.00 | 0.669 | Mo | 1 | 4 | 54 | 84 | 6027 | 0.0139 | 54.19 | 2.587 | Ag | 1 | 3 | 27 | 52 | 8446 | 0.0062 | 33.54 | 1.377 | W | 0 | 4 | 32 | 52 | 7237 | 0.0072 | 33.55 | 1.577 | Sn | 0 | 6 | 52 | 82 | 10429 | 0.0079 | 52.90 | 1.973 |
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Beneficial degree of each element anomaly
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| 证据图层 | W+ | W- | C | | 满克头鄂博组 | 1.342 | -1.119 | 2.461 | 地质变量 | 潜火山岩边界2 km缓冲区 | 0.436 | -0.659 | 1.094 | | 断裂450 m缓冲区 | 0.761 | -3.875 | 4.636 | | 断裂等密度 | 1.959 | -0.630 | 2.589 | | U高场 | 1.885 | -1.102 | 2.987 | 航放 | F参数高值晕 | 1.763 | -0.655 | 2.417 | | U/K高值晕 | 1.816 | -1.026 | 2.842 | | Hu低值晕 | 1.725 | -0.894 | 2.619 | 航磁 | 磁场有利区(-100~75 nT) | 0.023 | -0.267 | 0.290 | 化探 | Mo化探异常 | 1.813 | -0.773 | 2.587 | | Ag化探异常 | 1.061 | -0.316 | 1.377 | | Pb化探异常 | 1.240 | -0.427 | 1.667 | | W化探异常 | 1.250 | -0.327 | 1.577 | | Sn化探异常 | 1.332 | -0.641 | 1.973 | 遥感 | 铁染蚀变异常 | 0.526 | -0.522 | 1.049 | | 羟基蚀变异常 | 0.874 | -0.556 | 1.430 |
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Weight value of evidence layers of uranium deposits
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Prospective map of uranium mineralization in Linxi-Ulanhot area 1—regional fault、general fault;2—uranium deposit 、uranium occurrences、uranium mineralized site;3—volcanic basin and numbering;4—first prospective areas;5—second prospective areas;6—third prospective areas;7—prospective areas and numbering;8—study area
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