This review considers the magmatic processes in the Carpathian–Pannonian Region (CPR)
from Early Miocene to Recent times, as well as the contemporaneous magmatism at its …

The Pannonian Basin is a continental back-arc basin. Palaeomagnetics defined three
terranes: Alcapa (Alps–Carapathians–Pannonian), Tisza–Dacia and Dinarides, rotated …

" Department of Geophysics, Eötvös University, Budapest, 1085 Ludovika tér 2. Hungary
“Department of Engineering Geology, Technical University of Budapest, Stoczek u. 2 …

The palaeogeographic evolution of the Paratethyan and Mediterranean realms are
reconstructed with three maps ranging from the Late Miocene to the Middle–Late Pliocene …

The past decade has witnessed spectacular progress in the collection of observational data
and their interpretation in the Pannonian Basin and the surrounding Alpine, Carpathian and …

In the Carpathian–Pannonian region in Neogene times, westward-dipping subduction in a
land-locked basin caused collision of two lithospheric blocks (Alcapa and Tisia) with the …

The Miocene Central Paratethys Sea covered wide areas of the Pannonian Basin System,
bordered by the mountain chains of the Alps, Carpathians and Dinarides. The epicontinental …

The structure of the Pannonian basin is the result of distinct modes of Mid-Late Miocene
extension exerting a profound effect on the lithospheric configuration, which continues even …

The formation of the North Croatian Basin, which represents the south‐western marginal
part of the Pannonian Basin System and the Central Paratethys Bioprovince, began during …

Almandine garnet-bearing andesites and dacites occur frequently in the Neogene calc-
alkaline volcanic series of the northern Pannonian Basin (Hungary and Slovakia). They …