A5080784458- Geological Formations and Processes Exploration
- Geological and Geochemical Analysis
- Geology and Paleoclimatology Research
- Mineralogy and Gemology Studies
- Paleontology and Stratigraphy of Fossils
- Geotourism and Geoheritage Conservation
- Marine and environmental studies
- High-pressure geophysics and materials
- Geochemistry and Geologic Mapping
- Ancient and Medieval Archaeology Studies
- earthquake and tectonic studies
- Methane Hydrates and Related Phenomena
- Geological formations and processes
- Geological and Geophysical Studies Worldwide
- Pleistocene-Era Hominins and Archaeology
- Hydrocarbon exploration and reservoir analysis
- Dental Radiography and Imaging
- Geochemistry and Elemental Analysis
- Maritime and Coastal Archaeology
- Planetary Science and Exploration
- Paleontology and Evolutionary Biology
- Coal and Coke Industries Research
- Archaeological Research and Protection
- Chemical Thermodynamics and Molecular Structure
- Geomagnetism and Paleomagnetism Studies
Eötvös Loránd University
2016-2025
V. B. Sochava Institute of Geography
2021-2024
Volcano Corporation (United States)
2024
Hungarian Research Network
2022-2023
Research Network (United States)
2023
Institute for Geological and Geochemical Research
2019-2021
University of Palermo
2019
Institute for Soil Sciences
2017-2018
Pázmány Péter Catholic University
2007
Hungarian Academy of Sciences
2007
The Tokaj Mts. volcanism occurred in a thinning continental lithosphere regime at the final stage of subduction process. Using high-precision zircon U-Pb dating, four major explosive eruption events were distinguished. Among them 13.1 Ma Sátoraljaújhely and 12.0 Szerencs eruptions could have yielded large amount volcanic material (possibly > 100 km3) they associated with caldera collapse as shown by several hundred-metre-thick pyroclastic deposits long (>100 km) runout flow case eruption....
We report major and trace element abundances Sr, Nd Pb isotopic data for Miocene (16·5–11 Ma) calc-alkaline volcanic rocks from the western segment of Carpathian arc. This suite consists mostly andesites dacites; basalts basaltic as well rhyolites are rare occur only at a late stage. Amphibole fractionation both high low pressure played significant role in magmatic differentiation, accompanied by high-pressure garnet during early stages. Sr–Nd–Pb indicate crustal materials petrogenesis...
Abstract During Tertiary to Quaternary times, convergence between Eurasia and Africa resulted in a variety of collisional orogens different styles subduction the Alpine-Mediterranean region. Characteristic features this area include arcuate orogenic belts extensional basins, both which can be explained by roll-back subducted slabs retreating zones. After cessation active subduction, slab detachment post-collisional gravitational collapse overthickened lithosphere took place. This complex...
We present a novel approach to use zircon as correlation tool well monitor for magma reservoir processes in silicic volcanic systems. Fingerprinting eruption products based on trace element content and U-Pb dates of offers promising, previously underestimated tephra perspective, particularly cases where the main minerals glass are altered. Using LA-ICP-MS analyses, rapid cost-effective method, this study presents concentration data more than 950 crystals from scattered occurrences early...
Repeated explosive eruptions of large volume silicic magmas during the early-to mid-Miocene resulted in pyroclastic deposits covering at least 50,000 km 2 Pannonian Basin.They form extended marker horizons and therefore these formations have a great stratigraphic importance.Lithostratigraphic characterization classification rocks go back for more than century been used widely geological mapping among other things.In this paper, we outline former stratigraphical schemes developed products...
Abstract Loess–paleosol outcrops were logged and dated to trace loess cover during the Pleistocene in a low-elevation mountainous area. The exposed successions maximum of 15 m thick stratigraphically fragmentary. Still, results suggest that was deposited all climatically suitable periods within limits dating methods (ca. 400 ka), probably also beyond this. Luminescence measurements provided numerical ages from ca. 18 ka 200 minimum up >267 ka. Loess accumulation active relatively mild MIS...
Numerical models are essential tools for investigating a variety of Earth phenomena, providing insights into the role different surface to deep processes. As with many laboratory approaches effectiveness can be assessed by comparing their results natural case studies same phenomenon, which helps constrain large number model parameters.This presentation will take example Pannonian Basin system having been formed within Alpine–Carpathian–Dinaric orogenic belt, where...