Cargando…
Forecasting magma-chamber rupture at Santorini volcano, Greece
How much magma needs to be added to a shallow magma chamber to cause rupture, dyke injection, and a potential eruption? Models that yield reliable answers to this question are needed in order to facilitate eruption forecasting. Development of a long-lived shallow magma chamber requires periodic infl...
Autores principales: | Browning, John, Drymoni, Kyriaki, Gudmundsson, Agust |
---|---|
Formato: | Online Artículo Texto |
Lenguaje: | English |
Publicado: |
Nature Publishing Group
2015
|
Materias: | |
Acceso en línea: | https://www.ncbi.nlm.nih.gov/pmc/articles/PMC4623603/ https://www.ncbi.nlm.nih.gov/pubmed/26507183 http://dx.doi.org/10.1038/srep15785 |
Ejemplares similares
-
Breathing modes of Kolumbo submarine volcano (Santorini, Greece)
por: Bakalis, Evangelos, et al.
Publicado: (2017) -
Stratospheric Ozone destruction by the Bronze-Age Minoan eruption (Santorini Volcano, Greece)
por: Cadoux, Anita, et al.
Publicado: (2015) -
New insights into hydrothermal vent processes in the unique shallow-submarine arc-volcano, Kolumbo (Santorini), Greece
por: Kilias, Stephanos P., et al.
Publicado: (2013) -
Size distributions of fractures, dykes, and eruptions on Etna, Italy: Implications for magma-chamber volume and eruption potential
por: Scudero, Salvatore, et al.
Publicado: (2019) -
Depth of origin of magma in eruptions
por: Becerril, Laura, et al.
Publicado: (2013)