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The imprint of crustal density heterogeneities on regional seismic wave propagation

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Academic year: 2020

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Figure

Figure 1. The grid of receivers (black triangles) on the surface ofthe computational domain
Figure 2. Realisations of random density variations. Left: 200 km lateral correlation length, 20 km vertical correlation length
Figure 3. Comparison of synthetic seismograms for homogeneous and heterogeneous crustal densities in the broadest frequency band fromThe correlation lengths of the heterogeneities in velocities and density are 200 km in the horizontal and 20 km in the vert
Figure 4. Component-wise time shifts and relative amplitude differences in the frequency band from 0.02 to 0.04 Hz for five random mediarealisations.
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