Anna Vozárová

Comenius University Bratislava

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Co-Authors

J. Vozár

Slovak Academy of Sciences

KŠ

Katarína Šarinová

Comenius University Bratislava

НВ

Н. В. Родионов

Geological Institute

E. N. Lepekhina

A.P. Karpinsky Russian Geological Research Institute

I. P. Paderin

A.P. Karpinsky Russian Geological Research Institute

АН

А. Н. Ларионов

A.P. Karpinsky Russian Geological Research Institute

Fritz Ebner

Montanuniversität Leoben

Tibor Szederkényi

Eötvös Loránd University

Sándor Kovács

Eötvös Loránd University

Mirko Belak

Croatian Geological Survey

Cooperative Institutions

Geological Institute

State Geological Institute of Dionýz Štúr

Comenius University Bratislava

Centre National de la Recherche Scientifique

Slovak Academy of Sciences

A.P. Karpinsky Russian Geological Research Institute

University of Zagreb

Geological Survey of Slovenia

Eötvös Loránd University

Instytut Nauk Geologicznych

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Fluid inclusion and stable C-O isotope constraints on the origin of metasomatic magnesite deposits of the Western Carpathians, Slovakia

Russian Geology and Geophysics (2011)

Vratislav Hurai Monika Huraiová Peter Koděra Walter Prochaska Anna Vozárová

Metasomatism

Magnesite

Abiogenic petroleum origin

10.1016/j.rgg.2011.10.015

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Citations (15)

Stratigraphic correlations between the continental and marine Tethyan and Peri-Tethyan basins during the Late Carboniferous and the Early Permian

Geodiversitas (1998)

Raissa Kozitskaya Mahmoud Kora Dominique Massa D. Mercier Olivier Monod

The compilation of detailed stratigraphic, sedimentologic and paleontologic data resulted in stratigraphic correlations of marine and continental areas outcropping today in the Tethyan and Peri-Tethyan domains: (1) the base of the Moscovian would correspond to the base of the Westphalian C in the Peri-Tethyan domain and to the base of the Westphalian B in the Tethyan domain; (2) the Kasimovian, the Gzhelian and the Orenburgian would correspond in the northern Peri-Tethyan domain and Tethyan domain (Carnic Alps) respectively to the early Stephanian, the late Stephanian and the Autunian p.p., in the southern Peri-Tethyan domain to an undifferentiated time interval. The boundary between the Stephanian and the Autunian was recognized in the Donets Basin with some doubts; (3) the Asselian, Sakmarian, Artinskian and Kungurian would correspond in all the domains to the Autunian p.p. and the Saxonian that remain difficult to separate.

Westphalian sovereignty

Outcrop

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Citations (20)

Magnetostratigraphy of The Western-carpathians Permian (slovakia)

EGS General Assembly Conference Abstracts (2002)

Anna Vozárová I. Túnyi

Magnetostratigraphy

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Metabasic rocks from the Zemplinic crystalline basement (Western Carpathians, Slovakia): Metamorphic evolution and igneous protolith

Geologica Carpathica (2022)

Anna Vozárová Ondřej Němec Katarína Šarinová J. Vozár

Protolith

Basement

10.31577/geolcarp.73.6.6

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Citations (1)

Permian

Tom McCann Hubert Kiersnowski Karl Krainer Anna Vozárová Tadeusz Marek Peryt

This two-volume set provides the first comprehensive account in English of the geology of Central Europe. Written by more than 200 scientists from universities and research centres spread across Europe and North America, the 21 chapters are based on the main stratigraphic periods. Individual chapters outline the evolution of the region divided into a variety of sections which include overviews of the stratigraphic framework, climate, sea-level variations, palaeogeography and magmatic activity. These are followed by more detailed descriptions of the Central European succession, covering the main basins and magmatic provinces. Each chapter is thoroughly referenced, providing a unique and valuable information source.Volume 1 focuses on the evolution of Central Europe from the Precambrian to the Permian, a dynamic period which traces the formation of Central Europe from a series of microcontinents that separated from Gondwana through to the creation of Pangaea. Separate summary chapters on the Cadomian, Caledonian and Variscan orogenic events as well as on Palaeozoic magmatism provide an overview of the tectonic and magmatic evolution of the region. These descriptions sometimes extend beyond the borders of Central Europe to take in the Scottish and Irish Caledonides as well as the Palaeozoic successions in the Baltic region.Volume 2 provides an overview of the Mesozoic and Cenozoic evolution of Central Europe. This period commenced with the destruction of Pangaea and ended with the formation of the Alps and Carpathians and the subsequent Ice Ages. Separate summary chapters on the Permian to Cretaceous tectonics and the Alpine evolution are also included. The final chapter provides an overview of the fossil fuels, ore and industrial minerals in the region.The Geology of Central Europe is a key reference work suitable not only for libraries across the world, but of interest to all researchers, teachers and students of European Geology.

Pangaea

Palaeogeography

10.1144/cev1p.10

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Citations (20)

Permian of the West Carpathians : reports

J. Vozár Anna Vozárová Geologický ústav Dionýza Štúra

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Clastic wedge provenance in the Zemplinicum Carboniferous–Permian rocks using the U–Pb zircon age dating (Western Carpathians, Slovakia)

International Journal of Earth Sciences (2018)