This paper presents two-dimensional numerical models of the thermal structure of the crust and upper mantle in the Carpathians region based on new seismic data along the profile Dobre-3 (PANKACE) from East European Craton to Pannonian basin (PB). Heat flow and temperature distribution in the crust can be explained by lithosphere structure and Cenozoic tectonic and magmatic activity.
1. Kutas R.I. Teplovoe pole i geotermicheskij rezhim litosfery // Litosfera Central'noj i Vostochnoj Evropy. Obobshhenie rezul'tatov issledovanij (Gl. red.. A.V.Chekunov). – Kiev: Nauk. dumka, 1993. – S.114-135.
2. Kutas R.I., Cvjashhenko V.A., Korchagin I.N. Modelirovanie teplovogo polja kontinental'noj litosfery. – Kiev: Nauk. dumka, 1989. – 192 s.
3. Litosfera Central'noj i Vostochnoj Evropy. Geotraversy I, II, V / Gl. red. A.V.Chekunov. – 1988. – Kiev: Nauk. dumka. – 168 s.
4. Tektonichna karta Ukrainy. Poiasniuvalna zapyska. Masshtab 1:1000000 / Vidpov. red. D.S. Hurskyi, S.S. Kruhlov. – Kyiv: UkrDHRI. – 2007. – 96 s.
5. Starostenko V.I. et al. Seismic velocity model of the crust and upper mantle along profile PANCAKE across the Carpathians between the Pannonian Basin and the East European Craton / Tectonophysics. – 2013. – DOI: 10.1016/j.tecto.2013.07.008 https://doi.org/10.1016/j.tecto.2013.07.008