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The seismic velocity structure of the Wadati-Benioff Zone – insights from guided waves

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Figure

Figure 2.1 – Approximate ray path of guided and converted phases. The schematic figure clearly shows that guided wave phases spend longer interacting with the LVL than any other phase
Table 2.3 – Comparison of estimates of mineral bound H2O is the subducting plate. Amounts subducted quoted in Tg/Myr/m of arc
Figure 3.1 – Staggered grid for 2D FD scheme. a) The elastic variable distributed on the grid
Figure 3.2 – Approximation of a visco-elastic body using   Maxwell bodies. Modified from Emmerich & Korn, (1987) and Bohlen, (2002)
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