Abstract The Western Carpathians are separated into an Outer and Inner Carpathians (both
comprising several nappe systems) by the extremely narrow and highly deformed Pieniny …

Based on a self-consistent K–Ar database completed with up-to-date geochronological
information, this review paper addresses the general time–space evolution of Neogene …

To track the evolution and formation of one of the major sub-basins of the Pannonian back-
arc basin system, we re-evaluate pre-rift, syn-rift, post-rift, and inversion stages of the …

We report major and trace element abundances and Sr, Nd and Pb isotopic data for
Miocene (16· 5–11 Ma) calc-alkaline volcanic rocks from the western segment of the …

Geological mapping in volcanic terrains is a challenging task as there needs to be input from
various geologists' groups and only limited, often ambiguous guidelines exist. Volcanoes …

40Ar/39Ar radio-isotopic dating of volcanic tuffs intercalated in sediments can provide high
accuracy age control on the deposition of sedimentary rocks. State-of-the-art mass …

The Štiavnica Stratovolcano in Central Slovakia is the largest volcano in the Neogene to
Quaternary Carpathian volcanic arc. A large caldera, an extensive subvolcanic intrusive …

Abstract The Danube Basin represents a Miocene depocenter located on the NW margin of
the Alpine-Pannonian-Carpathian region and is considered a partial sub-basin of the larger …

A complex application of digital elevation model (DEM) derivatives is presented for a highly
degraded volcanic area, the Miocene Börzsöny Mountains, Hungary. We propose …

As a part of the long-standing volcanism of the Carpathian–Pannonian Region, a basaltic
monogenetic volcanic field developed here from 8–2.3 Ma. This is a specific type of …