The basins and orogens of the Mediterranean region ultimately result from the opening of
oceans during the early break-up of Pangea since the Triassic, and their subsequent …

The early Alpine tectonic evolution of the Western Carpathian orogenic system is
differentiated into four main periods:(i) Middle‐Late Triassic rifting and spreading of the …

The data on the Neogene geodynamics, palaeogeography, and basin evolution of the
Western Carpathians, Northern Pannonian domain and adjoining areas (ALCAPA Mega …

The data about the Paleogene basin evolution, palaeogeography, and geodynamics of the
Western Carpathian and Northern Pannonian domains are summarized, re-evaluated …

Abstract The Meliata Unit (Meliaticum) is a tectonic superunit of the Western Carpathians
that incorporates the blueschists-facies Bôrka Nappe and the low-grade metasediments and …

Abstract The Western Carpathian Meliata Superunit (Meliaticum) includes a heterogeneous
group of units—the blueschist-facies Bôrka Nappe and the very low-grade chaotic …

This study reports the Neotethyan Meliata Basin ophiolite fragments in the Late Jurassic–
Early Cretaceous accretionary wedge mélange in the southern part of the Inner Western …

Abstract The Cretaceous to Palaeogene Alpine exhumation of previously buried Variscan
basements is recorded in the southern portion of the Western Carpathians in the Gemeric …

This study presents petrological, geochemical, geochronological and structural data that
serve to identify two different Alpine tectonic units formed from the Variscan-aged Tribeč …

Abstract The Western Carpathians crystalline basement recorded common indications of the
Cadomian/Avalonian basement precursors. There the pre-Mesozoic basement of the Tatric …