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Magma chamber evolution during the 1650 AD Kolumbo eruption provides clues about past and future volcanic activity

Kolumbo submarine volcano lies 7 km NE of Santorini caldera and its last eruption which occurred in 1650 AD, caused damage and casualties to the nearby islands. Here a simple model of a chamber, containing silicic magma underlain by a smaller quantity of mafic magma, is utilised in order to understa...

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Detalhes bibliográficos
Publicado no:Sci Rep
Autor principal: Konstantinou, K. I.
Formato: Artigo
Idioma:Inglês
Publicado em: Nature Publishing Group UK 2020
Assuntos:
Acesso em linha:https://ncbi.nlm.nih.gov/pmc/articles/PMC7509795/
https://ncbi.nlm.nih.gov/pubmed/32963282
https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1038/s41598-020-71991-y
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