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 …

Plate motion and associated tectonics explain the location of magmatic systems along plate
boundaries [1], however, they cannot give satisfactory explanations of the origin of intra …

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

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 …

During Earth's history, geosphere-biosphere interactions were often determined by
momentary, catastrophic changes such as large explosive volcanic eruptions. The Miocene …

In protected areas (eg geoparks, UNESCO sites), the identification of the different aspects of
geoheritage site values is part of a holistic concept of protection, education and sustainable …

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 …

Volcaniclastic rocks are commonly used to date sedimentary series since absolute ages are
routinely obtained from several geochronological methods. In this work, we present five …

Repeated explosive eruptions of large volume silicic magmas during the early-to mid-
Miocene resulted in pyroclastic deposits covering at least 50,000 km2 in the Pannonian …

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 …