A Comment on “A major Change in the Stratigraphy of the Santorini Volcano in Greece”
Résumé
Friedrich and coauthors [1] propose that two prominent eruption deposits of Santorini Volcano are in fact the same unit, resulting in a major reinterpretation of the volcanic history of this caldera. Here I summarize published field and petrological evidence showing that their proposal is not correct.
Domaines
Volcanologie
Origine : Fichiers éditeurs autorisés sur une archive ouverte
