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The application of airborne time-domain electromagnetic method to the optimization and evaluation of copper and multi base-metals targets in New England Orogen, Australia |
Ming-Zuan XU, Yan HUANG, Jian-Sheng LIU, Jian-Dong LIU, Sheng-Yue LIANG, Feng CHEN, Jun-Cheng WANG |
Geological Exploration Technology Institute of Jiangsu Province, Nanjing 210049,China |
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Abstract The New England Orogen(NEO)is located in East Australia. Due to the numerous copper polymetallic deposits or ore spots and the complicated evolution history of tectonic activity, NEO shows the high exploration potential for copper polymetallic minerals, even large-sized deposits. The airborne electronic anomalies were delineated by airborne time-domain electromagnetic method. Based on the aerial electronic anomalies and using a method called "Seeking Common" with the known copper polymetallic ore spots, the authors performed the optimization and evaluation of copper polymetallic minerals in an exploration license within quite difficult topographic conditions for ground exploration in NEO. Using the airborne time-domain electromagnetic method, the authors rapidly and effectively determined and optimized nine copper polymetallic exploration targets. Those targets were classified into three levels: Level Ⅰ, Ⅱ, Ⅲ. Finally, and there were three, five and one targets for Level Ⅰ, Ⅱ, Ⅲ respectively. In a word, the work completed in this paper is expected to provide a referable case for rapidly and effectively conducting optimization and evaluation of copper polymetallic minerals in some special areas within difficult topographies for ground exploration both in China and abroad.
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Received: 09 August 2018
Published: 10 April 2019
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Geological conditions of working area 1—Quaternary;2—Paleogene basalt;3—Paleogene bandstone, conglomerate & mudstone;4—Permian shale & conglomerate; 5— Permian sand-mudstone; 6— Permian shale; 7— Permian siltstone & shale; 8—Permian lamellar conglomerate & siltstone; 9—Permian lamellar mudstine & slate; 10—perimian lamellar mudstone, sand-mudstone, sandstone & conglomerate;11—carboniferous conglomerate & sandstone-shale;12—tuffaceous conglomerate & paraconglomerate;13—tuffaceous paraconglomerate;14—tuffaceous sandstone-conglomerate;15—carbonatized tuffaceous sandstone & shale;16—welded dacitic tuff;17—fumarolic dacitic-andesitic tuff;18—welded tuff, paraandesite & rhyolite;19—welded tuff with rubble; 20—VTEM working area;21—known mineralized occurrence;22—inferred fault;23—measured fault;24—stream
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岩石名称 | 感应磁化强度/(4π×10-6 SI) | 剩余磁化强度/(10-3 A·m-1) | 极化率/% | 电阻率/(Ω·m) | 变化 范围 | 几何 平均值 | 变化 范围 | 几何 平均值 | 变化 范围 | 几何 平均值 | 变化 范围 | 几何 平均值 | 玄武岩 | 713.91~1437.79 | 972.62 | 4.10~10.15 | 5.45 | 2.60~52.6 | 27.60 | 12042~23135 | 13728 | 铅锌矿石 | 11.96~677.70 | 62.32 | 0~0.29 | 0.02 | 5.10~8.70 | 6.93 | 5354~43417 | 12212 | 流纹状凝灰岩 | 1.50~22.46 | 5.81 | — | — | 0.60~0.80 | 0.70 | 392~526 | 454 | 英安质 安山凝灰岩 | 2.01~1070.46 | 122.19 | 0.01~3.74 | 0.32 | — | 2.10 | — | 533 |
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发射 线圈 | 发射线圈直径:26 m 面积×匝数:2 123 m2 匝数:4 基本频率:25 Hz 电流峰值:190 A 供电时间:7.36 ms 波形:梯形 偶极距峰值:403 506 nIA 离地高度:70 m | 接收 线圈 | 接收线圈直径:1.2 m 面积×匝数:113.04 m2 匝数:100 |
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Working parameters of transmitting loop and receiver
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Constitution of VTEMPlus System
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Total Magnetic Polarization Plan for Working Area
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Time decay constan of dB/dt (Tau) contour of working area
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Comprehensive profiles of testing line L10450 a—Log dB/dt curve;b—strength of B field (channel 13~25);c—strength of B field (channel 25~37);d—strength of B field (channel 37~48);e—RDI of apparent resistivity;f—CDI of conductivity
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预测要素 | 描述内容 | 预测要 素分类 | 地质 环境 | 成矿区带 | 新英格兰后造山期岩浆成矿带 | 重要 | 地层 | 二叠纪的页岩、粉砂岩、杂砂岩,且伴有凝灰质火山岩 | 必要 | 火山岩 | 晚二叠世到早三叠世(印支期)凝灰质火山岩、安山岩、流纹岩等 | 重要 | 成矿时代 | 晚二叠世到早三叠世 | 重要 | 成矿环境 | 重要的成矿环境为海相沉积岩成岩阶段,特别是多次火山活动之间的相对平稳时期 | 必要 | 构造背景 | 矿床受NE向同生断裂,或其次级断裂(NW—NNE为主)控制,断裂为其含矿热液运移的主要通道 | 必要 | 矿点 地质 特征 | 矿物组合 | 黄铁矿、磁黄铁矿、闪锌矿及方铅矿为主,可见少量黄铜矿 | 重要 | 矿石结构构造 | 块状为主,其次为浸染状和网脉状 | 次要 | 热液蚀变 | 硅化、绿泥石 绿帘石化、绢云母化、千枚岩化等,部分地区还发育黄铁矿化、碳酸盐化 | 重要 | 控矿条件 | 晚二叠世到早三叠世含矿热液从构造通道上涌与海水混合成矿。控矿条件主要有NE向同生断裂及其次级断裂和海相沉积岩成岩作用 | 必要 | 物探 异常 特征 | 航磁 | 有异常分布表明有岩浆热液活动 | 次要 | 航电 | 早期道(第20、25道)和晚期道(第30、35道)航电异常位置吻合较好,且异常中心多为晚期道异常,外围则为早期道异常;总体来看,航电异常与已知矿或矿化点空间分布位置较为吻合 | 必要 |
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Final map of copper multi-metals minerals targeting assessment and optimization in working area 1—Quaternary;2—Paleogene basalt;3—Paleogene sandstone, conglomerate & mudstone;4—Permian shale & conglomerate; 5—Permian sand-mudstone; 6—Permian shale; 7—Permian siltstone & shale; 8—Permian lamellar conglomerate & siltstone; 9—Permian lamellar mudstine & slate; 10—Perimian lamellar mudstone, sand-mudstone, sandstone & conglomerate;11—carboniferous conglomerate & sandstone-shale;12—tuffaceous conglomerate & paraconglomerate;13—tuffaceous paraconglomerate;14—tuffaceous sandstone-conglomerate;15—carbonatized tuffaceous sandstone & shale;16—welded dacitic tuff;17—fumarolic dacitic-andesitic tuff;18—welded tuff, paraandesite & rhyolite;19—welded tuff with rubble; 20—VTEM working area;21—known mineralized occurrence;22—inferred fault;23— measured fault;24—numbers of electronic anomalies;25— channel 20 electronic anomalies (dB/dt);26—channel 25 electronic anomalies (dB/dt);27—channel 30 electronic anomalies (dB/dt);28—channel 35 electronic anomalies (dB/dt);29—numbers of magnetic anomalies; 30—metallogenic targets; 31—stream
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