Research Article

Characteristic Seismic Waves Associated with Cryosphere Dynamics in Eastern Dronning Maud Land, East Antarctica

Figure 6

Record section indicating a typical teleseismic event occurred at Kermadec Is. ( ; event#; eq012; modified after [23]). The vertical axis is the relative time measured from 14:01:30.0 (UTC) on January 21, 2002. Original (no filtered) traces for all station along the profile represent high signal-to-noise ratio. Very strong signals during 20–30 s are composed of direct P and possibly reverberations from the ice-sheet. Faint signals found in 50–60 s may be an S-P converted wave at the 660 km discontinuity just beneath the event (S660P).
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