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- W1656945497 abstract "The most prominent geomorphological features of the eroded Mio/Pliocene Bakony-Balaton Highland intraplate alkaline basaltic volcanic field are the semi-circular, lava capped buttes. The semi-circular distribution of lava flows indicates strong geomorphological control on lava flow emplacement and suggests that lava flows accumulated behind geographical barriers, such as a former tuff ring around the phreatomagmatic volcanoes. This is supported by the fact that often the large buttes, capped with thick lava flows, are accompanied by a strong negative Boguer-anomaly indicating mass deficit characteristic for country rock excavation and vent zone subsidence. The presence of pyroclastic rocks overlain by circular shaped lava flows resembles a pyroclastic facies that commonly fill phreatomagmatic volcanic craters, vents and conduits. At two locations (Badacsony and Halap) in the BakonyBalaton Highland Volcanic Field good exposures allow the examination of the relationships between lava lakes and the former tuff ring deposits, producing peperitic lava lake margins." @default.
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- W1656945497 date "2002-01-01" @default.
- W1656945497 modified "2023-09-27" @default.
- W1656945497 title "Interaction between lava lakes and pyroclastic sequences in phreatomagmatic volcanoes: Haláp and Badacsony, Western Hungary." @default.
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