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geological radar method
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geological radar method
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地质雷达法
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geological radar method
地质雷达法
通过发射高频电磁脉冲波,利用地下介质电性参数的差异,根据回波的振幅、波形和频率等运动学和动力学特征来分析和推断介质结构和物性特征的方法。是一种高效的浅层地球物理探测技术。
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