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Volcanic architecture, eruption mechanism and landform evolution of a Plio/Pleistocene intracontinental basaltic polycyclic monogenetic volcano from the Bakony-Balaton Highland Volcanic Field, Hungary
Authors:Gábor Kereszturi  Gábor Csillag  Károly Németh  Krisztina Sebe  Kadosa Balogh  Viktor Jáger
Institution:1. Department of Geology and Mineral Deposits, University of Miskolc, H-3515, Miskolc-Egyetemváros, Hungary
2. Department of Geological Research, Geological Institute of Hungary, Stefánia út 14, H-1143, Budapest, Hungary
3. Volcanic Risk Solutions, Institute of Natural Resources, Massey University, Private Bag 11 222, Palmerston North, New Zealand
4. Department of Geology, University of Pécs, Ifjúság ú. 6, 7624 Pécs, Hungary
5. Institute of Nuclear Research of the Hungarian Academy of Sciences, Bem-tér 18/C, H-4026, Debrecen, Hungary
6. Department of Mineralogy, Herman Otto Museum, Kossuth u. 13, H-3525, Miskolc, Hungary
Abstract:
Keywords:
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