signal-to-noise ratio teleseismic traces in the time period of 2009-2010 recorded by 49
stations that were temporarily deployed in the region. A standard H-κ stacking method is
employed to determine Moho depth from receiver functions, and then CCP stacking image
method is used to check continuity of Moho discontinuity. Good coherence of Moho depth in
the study with previous seismic results shows the Moho topography beneath the region is …