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comparison of
perturbations from a
standard whole-Earth
model shown at 1325 km
depth. Colour version
Plate 12(a). (e) A cross
section from the Aegean
(left) to Japan (right).
Colour version Plate 12(b).
Upper panels for (d) and
(e), are P-wave mode
based on travel times
from Bijwaard et al .
(1998). Lower panels are
degree 20 S-wave model
S20RTS based on
Rayleigh-wave dispersion
from Ritsema and van
Heijst (2000). Note the
different perturbation
scales and the different
resolutions for the two
images. (W. Spakman,
personal communication
2003.)
(e)
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