Conduit dynamics of the Rungwe Pumice eruption (Tanzania): From storage to fragmentation of phonolitic-trachytic magmas

The eruptive style of magma is shaped by both storage conditions and ascent processes. Peralkaline melts, with relatively high water concentrations and low viscosity, are expected to better resist magmatic fragmentation compared to peraluminous melts. However, trachytic and phonolitic magmas can sti...

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Библиографические подробности
Главные авторы:	Lorenzo Cappelli, Gianmarco Buono, Lucia Pappalardo, Thomas D. van Gerve, Olivier Namur, Vanessa N. Sielenou, Evelyne Mbede, Shimba Kwelwa, Edista Abdallah, Gerald G. J. Ernst, Karen Fontijn
Формат:	Artigo
Язык:	Inglês
Опубликовано:	Volcanica 2026-04-01
Серии:	Volcanica
Предметы:	explosive eruption peralkaline magmatism east african rift magma fragmentation rungwe volcano
Online-ссылка:	https://www.jvolcanica.org/ojs/index.php/volcanica/article/view/365
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Conduit dynamics of the Rungwe Pumice eruption (Tanzania): From storage to fragmentation of phonolitic-trachytic magmas

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