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Swiss Journal of Geosciences
Fig. 5 | Swiss Journal of Geosciences

Fig. 5

From: Crustal structure of the northern Dinarides and southwestern part of the Pannonian basin inferred from local earthquake tomography

Fig. 5

Three-dimensional resolution test using the checkerboard test method (triangles represent seismic stations). Left: depth slices of the synthetic model. Right: inversion slices for the same depth. A checkerboard pattern with positive and negative velocity anomalies is superimposed on the initial velocity model, which is used for the final model. The locations of profiles that are presented in Fig. 6 are shown on the 18 km depth slice of the synthetic model. Areas of poor resolution are blanked

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