Fig. 8From: Crustal structure of the northern Dinarides and southwestern part of the Pannonian basin inferred from local earthquake tomographyDepth slices across the P-wave inversion model. HDB high-density body from Šumanovac (2010), marked by a solid black line; HV high-velocity anomaly, LV low-velocity anomaly. Triangles denote seismic stations. Positions of two vertical cross sections are shown in the 20 km depth slice. All anomalies marked here are superimposed on the tectonic map in Fig. 11Back to article page