在泥石流调查中,查清泥石流区域覆盖层厚度及基岩分界面对泥石流地质灾害的评价非常重要。该文将浅层瞬变电磁法用于北京市某地泥石流勘察中,特别是在场地受限、接地条件极差的区域,该方法显示了优越性。经过钻探和探坑的验证,浅层瞬变电磁法探测取得了令人满意的效果,是泥石流勘察的一种新方法。 In the debris flow survey, it is very important to find out the thickness of the cover layer in the debris flow area and the evaluation of the geological disasters of the bedrock flow interface. In this paper, the shallow transient electromagnetic method is applied to the debris flow exploration in a certain place in Beijing, especially in the area with limited site and poor grounding conditions. This method shows the superiority. After drilling and exploration pit verification, shallow transient electromagnetic detection has achieved satisfactory results, is a new method of debris flow exploration.