Defining Pre-eruptive Conditions of the Havre 2012 Submarine Rhyolite Eruption Using Crystal Archives
The 2012 Havre eruption evacuated a crystal-poor rhyolite (∼3–7% crystals) producing a volumetrically dominant (∼1.4 km3) pumice raft, as well as seafloor giant pumice (5–8%) and lavas (12–14%) at the vent (∼0.1 km3), both of which have subtly higher phenocryst contents. For crystal-poor rhyolites l...
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| Principais autores: | , , , |
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| Formato: | Artigo |
| Idioma: | Inglês |
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Frontiers Media S.A.
2020-07-01
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| coleção: | Frontiers in Earth Science |
| Assuntos: | |
| Acesso em linha: | https://www.frontiersin.org/article/10.3389/feart.2020.00310/full |
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