本文主要讨论超声物理模拟实际单层复杂地质结构的实验结果。在描述了采用的仪器装备,模型装置,测纲布置及观测方式之后,着重分析了复杂地质结构条件下模型实验的记录特点,指出单层界面可以在时间剖面上反映“多个”同相轴。这种现象说明了复杂构造地区时间剖面解释的复杂性,且要十分重视“特殊波” 的研究。 This paper mainly discusses the experimental results of simulating the actual single-layer complex geological structure by ultrasonic physics. After describing the equipment, model devices, layout and observation methods, the characteristics of the model experiment under complex geological conditions are analyzed. It is pointed out that the monolayer interface can reflect the “multiple” events in the time profile. This phenomenon illustrates the complexity of the interpretation of the time profile in complex tectonic regions, and attaches great importance to the study of “special waves.”