Results 221 to 230 of about 2,053 (253)
A new view is presented of the Bakony-Balaton Highland Volcanic Field (BBHVF), Hungary, active in late Miocene and built up of ca. 100 mostly alkaline basaltic eruptive centers, scoria cones, tuff rings, maar volcanic complexes and shield volcanoes.
Karoly Nemeth, Ulrike Martin
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Physical volcanology and eruption dynamics of peralkaline agglutinates from Pantelleria
Journal of Volcanology and Geothermal Research, 1997Peralkaline rhyolitic lava-like lobes showing direct evidence for a spatter-fed origin are associated with eruptive centres that document a transition from explosive to effusive fountain-fed activity. Owing to the preservation of spatter clasts, clast dimensions can be used to model the eruptive dynamics of these deposits.
Stevenson, R., Wilson, Lionel
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Physical volcanology of the Gubisa Formation, Kone Volcanic Complex, Ethiopia
Journal of African Earth Sciences, 2014Despite their significance for understanding the potential environmental factors involved in hominin evolution in Ethiopia, very few modern volcanologic studies have been carried out on the Quaternary calderas and associated silicic tephra deposits of the Ethiopian Rift.
Michael L. Rampey +3 more
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The AD 1362 Öræfajökull eruption, S.E. Iceland: Physical volcanology and volatile release
Journal of Volcanology and Geothermal Research, 2008Abstract The explosive rhyolitic eruption of Oraefajokull volcano, Iceland, in AD 1362 is described and interpreted based on the sequence of pyroclastic fall and flow deposits at 10 proximal locations around the south side of the volcano. Oraefajokull is an ice-clad stratovolcano in south central Iceland which has an ice-filled caldera (4–5 km ...
Kirti Sharma +4 more
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Journal of Volcanology and Geothermal Research, 2008
Abstract The Ferrar Large Igneous Province forms a linear belt for 3500 km along the Transantarctic Mountains, and as a geochemical province extends into southeastern Australasia. The principal components of the Ferrar are: intrusive — Ferrar Dolerite sills and dikes, and Dufek intrusion; pyroclastic — the Prebble, Mawson and Exposure Hill Formations;
D.H. Elliot, T.H. Fleming
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Abstract The Ferrar Large Igneous Province forms a linear belt for 3500 km along the Transantarctic Mountains, and as a geochemical province extends into southeastern Australasia. The principal components of the Ferrar are: intrusive — Ferrar Dolerite sills and dikes, and Dufek intrusion; pyroclastic — the Prebble, Mawson and Exposure Hill Formations;
D.H. Elliot, T.H. Fleming
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Physical Volcanology of the Cora Maar, Erciyes Volcanic Complex
2005WOS ...
Atilla, Cineyt, Gencalioglu Kuscu, Gonca
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The Tectonics and Physics of Volcanoes. Journal of Volcanology and Geothermal Research, 144
2005The tectonics and physics of volcanoes. Structural control of volcanism and caldera development in the transtensional Taupo Volcanic Zone, New Zealand. Structural setting of the Bicol Basin and kinematic analysis of fractures on Mayon Volcano, Philippines.
GUDMUNDSSON A. +2 more
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Why the Tongan eruption will go down in the history of volcanology
Nature, 2022Witze Alexandra
exaly
PHYSICAL VOLCANOLOGIC EVOLUTION OF AN AGGLUTINATED CRATER RIM SEGMENT
Geological Society of America Abstracts with Programs, 2017Samuel Xavier Hudziak +4 more
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Physical volcanology of Surtsey, Iceland: A preliminary report
Surtsey research, 2000openaire +1 more source

