| 木利锑矿三家村测区构造地球化学及找矿远景 |
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| 引用本文： | 张勤,杨玉华.木利锑矿三家村测区构造地球化学及找矿远景[J].云南地质,2012(3):368-373. |
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| 作者姓名： | 张勤 杨玉华 |
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| 作者单位： | 云南有色地质局308队 |
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| 摘 要： | 南北向右行扭动构造体系控制金、锑矿分布。泥盆系锑异常规模大、强度高、浓集中心明显;金异常零星分布于三叠系、寒武系中,规模小。金、砷、锑元素组合为金矿矿致异常。三家村南东段浅部找锑深度找金;西洋河段浅部找与硅质岩有关的金,翠峰上组找第二层金(锑)矿。
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| 关 键 词： | 低温热液锑金矿 构造交汇部位 泥盆系锑异常 三叠系金异常 云南广南木利 |
THE STRUCTURE GEOCHEMISTRY AND PROSPECTING POTENTIALITY OF SANJIACUN AREA OF MULI SB OREFIELD |
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| ZHANG Qin,YANG Yu-hua.THE STRUCTURE GEOCHEMISTRY AND PROSPECTING POTENTIALITY OF SANJIACUN AREA OF MULI SB OREFIELD[J].Yunnan Geology,2012(3):368-373. |
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| Authors: | ZHANG Qin YANG Yu-hua |
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| Institution: | (Geological Team 308,Yunnan Bureau of Nonferrous Geology,Gejiu 616400) |
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| Abstract: | The distribution of Au,Sb deposit is controlled by the NS right-handed torsion structure system.The Devonian Sb anomaly is in large scale,high intensity,with the clear concentration center,whereas the scattered Au anomaly is distributed in Triassic,Cambrian,in small scale.There are a series of prospecting trace,such as,Au,As,Sb assemblage anomaly;Sb in shallow,Au in deep of SE Sanjiacun Member;Au related to silicic rock in shallow of Xiyanghe Member;Au(Sb)in 2nd bed of Cuifengshan Formation. |
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| Keywords: | Low T Hydrothermal Sb(Au)Deposit Structure Intersection D Sb Anomaly T Au Anomaly Muli Guangna Yunnan |
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