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The application of integrated geophysical method to the exploration of Guanzixia graphite ore deposit in M area of Huining County |
SUN Hai-Chuan1, XU Xing-Rong2, WANG Ya-Feng1 |
1. Gansu Coal Geological Prospecting Institute, Lanzhou 730000,China 2. No.1 Geological Prospecting Institute, Gansu Bureau of Geology and Mineral Resources Exploration and Development, Tianshui 740020, China |
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Abstract The Guanzixia M exploration area in Huining County is located in the hilly and gully area of the Loess Plateau,which has a good prospect of prospecting for graphite ore. Firstly, graphite ore metallogenic conditions in the exploration area are analyzed. Then, the geophysical work is carried out in the favorable area of graphite mineralization. Adopting the dual frequency induced polarization intermediate gradient to measure the apparent amplitude frequency, apparent resistivity and the natural electric field adopted to measure natural,the two methods are used to delineate graphite mineralization anomalies,which are characterized by high amplitude frequency, low apparent resistivity and negative anomaly of natural potential. On this basis, the induced polarization sounding is used to find out the spatial distribution characteristics of mineralized anomalous bodies, and provides evidence for drilling through various methods. It has been verified by drilling that 2 layers of graphite ore are drilled, and obtained good exploration results.
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Received: 11 March 2020
Published: 27 July 2021
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Geological and geophysical engineering layout of the exploration area
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组别 | 岩石名称 | 标本 块数 | ρ/(Ω·m) | η/% | 最小值 | 最大值 | 平均值 | 总均值 | 最小值 | 最大值 | 平均值 | 总均值 | 1 | 褐红色长石岩屑细砂岩 | 9 | 1533 | 2420 | 1852 | | 0.63 | 0.94 | 0.75 | | 2 | 褐红色长石岩屑细砂岩 | 5 | 933 | 1125 | 1035 | | 0.48 | 0.52 | 0.5 | | 3 | 褐红色长石岩屑细砂岩 | 3 | 227 | 237 | 232 | 710 | 1.69 | 2.53 | 2.03 | 1.34 | 4 | 褐红色长石岩屑细砂岩 | 4 | 315 | 348 | 328 | | 1.12 | 1.28 | 1.19 | | 5 | 褐红色长石岩屑细砂岩 | 8 | 459 | 915 | 744 | | 1.82 | 2.25 | 2.07 | | 6 | 褐红色长石岩屑细砂岩 | 3 | 68.89 | 69.05 | 68.98 | | 1.99 | 1.08 | 1.5 | | 7 | 含砾石英粗砂岩 | 3 | 482 | 497 | 489 | | 1.31 | 1.4 | 1.36 | | 8 | 含砾石英粗砂岩 | 4 | 134 | 135 | 134 | | 1.93 | 1.05 | 1.41 | | 9 | 含砾石英粗砂岩 | 4 | 94.78 | 106.5 | 98.94 | 741.78 | 2.14 | 3.43 | 2.49 | 1.52 | 10 | 含砾石英粗砂岩 | 4 | 2746 | 3205 | 2897 | | 0.56 | 0.61 | 0.6 | | 11 | 含砾石英粗砂岩 | 3 | 89.22 | 90.95 | 89.96 | | 1.67 | 1.86 | 1.75 | | 12 | 石墨矿(化)石 | 3 | 136 | 138 | 137 | | 5.7 | 5.83 | 5.75 | | 13 | 石墨矿(化)石 | 4 | 76 | 82 | 79 | 86.59 | 2.51 | 3.11 | 2.83 | 4.64 | 14 | 石墨矿(化)石 | 3 | 43.65 | 43.88 | 43.78 | | 4.85 | 5.73 | 5.35 | |
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Statistical data table of physical properties of rock (mine) stone outcrop in exploration area
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Comprehensive section of 1 and 2 lines natural potential and dual frequency IP intermediate gradient measurement
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Sketch map of river filtering electric field
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Comprehensive section of 1 and 2 lines induced polarization sounding
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