Figure 10 depicts an increasing trend in the east–west cumulative deformation of observation points within the Maojiayu landslide, whereas the Taohuasi landslide area shows a more pronounced increasing trend in east–west cumulative deformation, though the overall magnitude of deformation remains small.
← all excerpts
Three-dimensional surface deformation field monitoring and influencing factors analysis in mountainous areas based on SBAS-INSAR technology (Tianjin, China).
1
—
—