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Earth, Planets and Space
Fig. 5 | Earth, Planets and Space

Fig. 5

From: Systematic difference between first-motion and waveform-inversion solutions for shallow offshore earthquakes due to a low-angle dipping slab

Fig. 5

Simulated waveforms derived from 2D simulations with varying dip angles θ of the subducting slab. Schematic figure of the model used is shown in upper left corner. Blue, red solid, and dashed lines represent direct P, P PHS, and Pn phases, respectively. Physical parameters of the assumed slab are listed in right bottom corner

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