Abstract The Dinarides and Carpathian-Balkans, the western Balkan Peninsula, form an essential link between the Paleotethyan branches of the Adriatic Sea (Montenegro, Croatia) …
Abstract The Eastern European lithosphere is a natural laboratory to study continental formation and evolution through time, comprising Archean continental remnants, Proterozoic …
Geometrical heterogeneity of the subducting Indian continental crust along the Himalaya‐ Tibet collision zone remains enigmatic. Mass budget estimates describing shortening across …
A wide range of volcanic rocks formed in the Carpathian–Pannonian region during the last 20 Myr, closely associated with the tectonic evolution of the area:(1) high-SiO2 rhyolites and …
Abstract The Tokaj Mts. volcanism occurred in a thinning continental lithosphere regime at the final stage of the subduction process. Using high-precision zircon U-Pb dating, four …
This paper presents the results from a geographic information systems (GIS) workflow, which was used to analyze the spatial distribution and temporal evolution of volcanoes in the Mio …
This study focuses on upper mantle xenoliths from Sabar-hill (Bakony-Balaton Highland Volcanic Field), a newly discovered locality of mantle xenoliths, situated in the central …
The subsidence history and sedimentary architecture of extensional basins are controlled by the interplay between tectonics, mantle dynamics and climatic variations. Observations from …
A NOVÁK, T RUBÓCZKI… - Geologica …, 2024 - pdfs.semanticscholar.org
The transition area between the Pannonian Basin and the East Carpathians is the subject of considerable tectonic research in Central Europe because of its geological diversity …