Abstract Knowledge about the crustal thickness is one of the key elements in the
reconstruction of the regional tectonic history. The Dinaric mountain belt is one of the most …

The nature of the interaction between Adriatic and Euroasian lithospheric plates in the
Dinarides is important for understanding the complex tectonic history of the central …

Broad-band seismograms of teleseismic events recorded at the Croatian Seismological
Network were used to compute radial receiver functions (RFs) for eight locations in the …

The study area covers the Dinarides and southwestern part of the Pannonian basin as the
marginal zone between the Adriatic microplate (African plate) and the Pannonian tectonic …

We present the results of local earthquake tomography (LET) analysis to investigate the
crust and uppermost mantle structure in the northern Dinarides and southwestern …

We present a new data set of Moho depth estimates for peninsular Italy, obtained from
receiver functions analysis and a grid search approach. Teleseismic records from 174 …

Passive seismic experiment was carried out at the SW contact of the Dinarides and
Pannonian basin to determine the crustal structure and velocity discontinuities. The aim of …

The interaction between the Adriatic microplate (Adria) and Eurasia is the main driving factor
in the central Mediterranean tectonics. Their interplay has shaped the geodynamics of the …

The area of study covers the marginal zone between the Adriatic microplate (African plate)
and the Pannonian segment (Eurasian plate). We present a tomography model for this area …

A gravity model has been established at the contact of the southern part of the Pannonian
basin and central Dinarides. Two-dimensional gravity modelling was carried out by means …