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作 者:黄华高[1] HUANG Hua-gao(No.1 Institute of Hydrogeological and Engineering Geological Exploration,Bureau of Geology and Mineral Exploration of Anhui Province,Bengbu,Anhui 233000,China)
机构地区:[1]安徽省地质矿产勘查局第一水文工程地质勘查院,安徽蚌埠233000
出 处:《安徽地质》2022年第1期56-58,83,共4页Geology of Anhui
摘 要:结合已知地质成矿规律,通过地面高精度磁测工作查明勘查区范围内的隐伏性岩体的分布;通过大功率激电中梯扫面和激电测深查明勘查区范围内与成矿有关的金属硫化物的分布及向下延伸状况,确定埋藏深度不大;通过磁法、激电中梯、激电测深工作,几处异常都呈现相对高磁-高极化率的反映,推断有成矿的可能,建议在加强地质论证的基础上实施钻孔验证工作。Based on the known geological and metallogenic regularity, the distribution of concealed rock masses in the work area was determined by high-precision magnetic surveying on the ground. The distribution and downward extension of metal sulfides related to mineralization in the work area were found by high-power IP intermediate gradient method scanning and IP sounding, and the burial depth was found small. Through magnetic method, IP intermediate gradient method and IP sounding,several anomalies show relatively high magnetism and high polarizability, and are thought to be related to mineralization. A drilling test was suggested after strengthened geological demonstration.
关 键 词:磁异常特征 激电异常分布特征 找矿预测 安徽铜陵
分 类 号:P63[天文地球—地质矿产勘探]
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