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Contribution to the numerical estimation of earthquake ground motions

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Academic year: 2021

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Figure

Figure II.21. Surface map of the central part of the Mygdonian basin, showing the accelerometric stations of the Euroseistest array (red triangles) and the epicentral locations of six local seismic events (beach-balls) which were used for the first stage o
Figure II.23. Values of misfit between synthetics and recordings for one of the six local events (the epicentre of which is indicated by the black star in the top left figure) retained in the first validation phase of E2VP
Figure II.24. Comparison of average absolute misfit values between different numerical predictions (blue circles) and between individual predictions and recordings (yellow, red and purple) for different sets of sources and real stations or receivers: (a) a
Figure II.30. Example of horizontal ground velocity computed for a large (W=20 km), deep (H=1 km), and soft (V S =125 m/s) valley with gentle edge slope (10 ◦ )
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