Research on Internal Structure and Mechanism of Landslide Based on Hydrogeophysical Investigation (Quan’an Landslide, Southwest China)

Figure 18

Ground penetrating radar results. The three abnormal areas A, B, and C in the west-east direction basically correspond to the three low-resistance abnormal areas near the surface of the autumn survey results, and the abnormal reflection points of D and E in the north-south direction basically correspond to the two low-resistance abnormal areas near the surface of the resistivity profile.