hrvatski

Kristalina podloga južnih dijelova Panonskog bazena-temeljena na površinskim i bušotinskim podacima

The basement of the South Pannonian Basin can be divided into four megablocks. 1) The largest South Tisia (Slavonija and Moslavina) megablock, composed mainly of Paleozoic metamorphic sequences, migmatites and granites. 2) The slightly smaller North Dinaridic megablock, composed of Late Cretaceous-Paleogene flysch, Paleogene metamorphic sequences, synkinematic granites and tectonized ophiolite melange. 3) The much smaller Zagorje-Midtransdanubia megablock, consisting of mixed tectonostratigraphic units from the Southern Alps and northwestern Dinarides. 4) The smallest Pohorje-Međimurje megablock, composed of tectonostratigraphic units from the Eastern Alps and Periadriatic zone. In the final part of paper is presented geodynamic evolution of the South Pannonian Basin.

Kristalina podloga; megablock;.geodinamska evolucija

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