浅层折射波法在工程地震勘探中早已成为普遍运用的常规物探方法,过去我们运用这种方法解决了许多工程地质问题,用得最为广泛的是探测基岩面埋深及其形态。随着物探技术的发展,对物探资料的综合分析利用开辟了广阔的前景,近年来我们在解决上述任务的同时,利用相遇互换时距曲线的界面速度曲线确定基岩的完整性,特别是圈定 Shallow refracted wave method has long been a commonly used method of conventional geophysical exploration in engineering seismic exploration. In the past, we used this method to solve many engineering geological problems. The most widely used method is to detect the depth and shape of the bedrock surface. With the development of geophysical exploration techniques, broad prospects have been opened up for the comprehensive analysis and utilization of geophysical data. In response to these tasks, we have also used the interfacial velocity curves of interchangeable time curves to determine the integrity of the bedrock, especially Delineated