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Indication significance of in-situ IP in exploration of concealed copper deposits |
Bao-Lin XUE1, Gui-Mei LIU2, Zeng-Biao TIAN1, Qiang ZHAO1, Lei REN1, Xin-Xue XU2, Jin-Qiang FU1 |
1. No. 519 Geological Party of North China Geological Exploration Bureau, Baoding 071051, China 2. Tianjin Geophysical Exploration Center, Tianjin 300170, China |
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Abstract In-well IP is one of the effective means to explore deep sulfide-type metal ore. In the well, the electric field-well method is used to find the bottom of the well and the blind mine near the well; in the well, the electric well-ground method is used to determine the ore body’s direction and judge its occurrence. The exploration examples of the Beiwopu copper deposit in Inner Mongolia indicate that the ground-well IP measurement corresponds to high polarization anomalies in the pyrite-rich and brass mineralization-enriched rock sections; the well-ground charging method is used to measure the occurrence of ore bodies. Judging, retrieving the direction of the ore body, guiding the drilling project, reducing the investment in exploration, and achieving A better prospecting effect.
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Received: 16 September 2019
Published: 24 June 2020
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Theoretical curve of ore bodies with different occurrences near the well
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ΔV2 curve of the ore body on the left side of the borehole
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ΔV2 curve of the ore body on the right side of the borehole
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序号 | 岩石名称 | 标本数 | 磁化率/(10-6SI) | 变化区间 | 平均值 | 1 | 闪长岩(含Cu、Fe矿化) | 34 | 3010~28900 | 12457 | 2 | 正长斑岩 | 34 | 239~1190 | 605 | 3 | 闪长岩 | 37 | 35~573 | 121 | 4 | 流纹岩 | 40 | 1340~7740 | 4597 | 5 | 玄武岩 | 34 | 3780~11700 | 7081 | 6 | 砂岩 | 35 | 35~128 | 76 | 7 | 板岩 | 35 | 274~1510 | 650 | 8 | 花岗岩 | 34 | 74~924 | 359 | 9 | 花岗闪长岩 | 30 | 67~175 | 107 | 10 | 花岗斑岩 | 30 | 114~451 | 221 |
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Rock magnetic parameter statistics table
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序号 | 岩石名称 | 标本数 | 极化率/% | 电阻率/(Ω·m) | 变化范围 | 平均值 | 变化范围 | 平均值 | 1 | 闪长岩(含Cu、Fe矿化) | 28 | 1.75~9.35 | 3.56 | 420~8714 | 3995 | 2 | 正长斑岩 | 34 | 0.36~2.19 | 1.30 | 657~9026 | 3089 | 3 | 闪长岩 | 36 | 0.64~2.08 | 1.43 | 408~9550 | 3942 | 4 | 流纹岩 | 36 | 0.35~2.67 | 1.04 | 555~4650 | 1982 | 5 | 玄武岩 | 30 | 0.76~6.07 | 2.0 | 272~8619 | 4241 | 6 | 砂岩 | 30 | 0.18~1.75 | 0.92 | 219~3705 | 920 | 7 | 板岩 | 30 | 0.16~1.56 | 0.82 | 252~2448 | 1169 | 8 | 花岗岩 | 30 | 0.64~2.71 | 1.6 | 322~4530 | 1304 | 9 | 花岗闪长岩 | 30 | 0.22~2.04 | 1.12 | 213~2516 | 1361 | 10 | 花岗斑岩 | 30 | 0.74~2.56 | 1.55 | 762~8817 | 2303 |
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Statistics of rock electrical parameters
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ZKW0001 well in the electromagnetic measurement curve
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Well-ground charging method visual polarization section interpretation map
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