Figure 2From: Dominant role of temperature on deep earthquake mechanics for the Tonga slab near the bottom of the upper mantleExamples of slant stack vespagrams for selected events. (Top) EV9 (Table 1) recorded at the Hi-net. Seismograms are phase-weight stacked with n=1 (Schimmel and Paulssen [1997]), and the color shows the stacked intensity (the strongest signals are red). The horizontal axis is the delay time (Δ t) in seconds after the first peak of the direct P wave. The vertical axis is the slowness relative to the direct P wave (Δ p) in seconds per degree. Arrival of the X phase (s-to-P reflected wave at horizontal interface above the foci) is seen near 8 s after P (s641P, Table 1). The predictions of s-to-P based on ak135 are marked with blue dots for every 5 km of interface depth. The stack outputs between 3 to 10.5 s after P are magnified 20 times, while those after 10.5 s are magnified 40 times. (Bottom) Same as the top panel, for EV8, showing the arrival of s639P (Table 1). The outputs after 4.5 s after P are magnified 30 times.Back to article page