Fig. 10

Alp07 cross-section through the P-wave inversion model with superimposed features defined in the 2D model. The topography is shown on the top, and the triangles denote seismic stations. HV high velocity, LV low velocity. The solid blue and red lines are crustal and Moho discontinuities inferred from the velocity model established by controlled-source experiments along the Alp07 profile of the ALP 2002 experiment (Šumanovac et al. 2009). The grey solid line represents the Moho inferred from receiver function modelling (Šumanovac et al. 2016). The dashed blue and red lines are discontinuities interpreted on the basis of our LET model. The dashed black line denotes the estimated mean depth for the Moho obtained by combining all three models. Note the vertical exaggeration. Numbers in green colour denote V_p seismic velocities from the 2D seismic refraction model, while HDB and crustal faults are represented by solid green and red dotted lines, retrospectively (Šumanovac et al. 2009)