Abstract Basic principles and techniques for the shallow seismic refraction wave method and the highdensity resistivity method
are described in this paper in combination with engineering practice to explain the results of the refraction wave method and the
high-density resistivity method in railroad and highway tunnel exploration. The application effects of the combination of these two
methods in detecting positions, sizes, natures and characteristics of such harmful geological bodies as concealed faults and shatter
zones are also discussed. Some measures for improving the investigation accuracy of these two methods are put forward.
|