What do you suggest that
implications of more stations to record earthquake data in Saudi Arabia will
help in imaging the crustal structures? And what do you think that the crustal
model suggested by the author and described in Table2 can be improved as it
already shows a lot of velocity variations in the crustal layers?
When do the Nyquist
frequency cause aliasing while digitization? What do you think?
If we consider
the assumptions regarding the vertical velocity gradient and lateral velocity
variations, the solutions to elastodynamic equation becomes easy or very
GPS readings alone appropriate to determine plate motions?
How would we be able to construct a reliable model for plate movement when
geodetic coverage is not equally distributed over the earth?