Magma evolution inside the 1631 Vesuvius magma chamber and eruption triggering

Autor: Stoppa F.[1], Principe C.[2], Schiazza M.[1], Liu Y.[3], Giosa P.[2, Crocetti S.[2

Publikováno v: Open Geosciences, Vol 9, Iss 1, Pp 24-52 (2017)
Open Geosciences 9 (2017): 24–52. doi:10.1515/geo-2017-0003
info:cnr-pdr/source/autori:Stoppa F.[1], Principe C.[2], Schiazza M.[1], Liu Y.[3], Giosa P.[2,4], Crocetti S.[2,4]/titolo:Magma evolution inside the 1631 Vesuvius magma chamber and eruption triggering/doi:10.1515%2Fgeo-2017-0003/rivista:Open Geosciences/anno:2017/pagina_da:24/pagina_a:52/intervallo_pagine:24–52/volume:9

Vesuvius is a high-risk volcano and the 1631 Plinian eruption is a reference event for the next episode of explosive unrest. A complete stratigraphic and petrographic description of 1631 pyroclastics is given in this study. During the 1631 eruption a

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_dedup___::53a625f93be7715438d9936b4d21bb3c
https://doaj.org/article/4a523ac97c404ee5931335e84930de15