Figure 7.

(a) the vertical crustal deformation rates in northeastern Tibet without the loading effect (from GRACE). Blue vectors denote uplift, and red vectors denote subsidence. The active faults in Tibet are marked by gray lines, and the black lines with triangles show two subduction belts in the northern and southern boundaries of Tibet; (b) profile charts showing the terrain height and uplift rate of the northeast Tibetan Plateau, the magenta dotted line from A to B in (a). The blue dots with error bars denote GPS sites with positive uplift rates and the red dots denote negative rates. The error bars represent one standard deviation on either side of the plotted points.