The Solfatara Magmatic-Hydrothermal System Geochemistry, Geothermometry and Geobarometry of Fumarolic Fluids

Autor: Marini L.[1], Principe C.[2], Lelli M.[2]

Publikováno v: Basel: Springer, 2022
info:cnr-pdr/source/autori:Marini L.[1], Principe C.[2], Lelli M.[2]/titolo:The Solfatara Magmatic-Hydrothermal System Geochemistry, Geothermometry and Geobarometry of Fumarolic Fluids/editore: /anno:2022

Solfatara volcano is situated close to the center of the Campi Flegrei caldera which, in the past, has alternatively experienced phases of resurgence and subsidence, traditionally indicated with the term bradyseism. Ludovico Sicardi (1895-1987) was a

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=cnr_________::90db82dfd3417d3a4750a2fecf7e46dd
https://www.springer.com/series/11157

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

Facies vulcaniche e meccanismi di messa in posto delle vulcaniti del Monte Amiata

Autor: Vezzoli L.M.[1, Principe C.[2]

Publikováno v: Il Vulcano di Monte Amiata, edited by a cura di Claudia Principe, Guido Lavorini e Luigina M. Vezzoli, pp. 195–214, 2017
info:cnr-pdr/source/autori:Vezzoli L.M.[1,2], Principe C.[2]/titolo:Facies vulcaniche e meccanismi di messa in posto delle vulcaniti del Monte Amiata/titolo_volume:Il Vulcano di Monte Amiata/curatori_volume:a cura di Claudia Principe, Guido Lavorini e Luigina M. Vezzoli/editore:/anno:2017

Mount Amiata is a silicic Quaternary volcano that poses the problem on the genetic interpretation of its products. The major volcanological arguments debated on Amiata, during the last 55 years, is the occurrence of explosive eruptions and the emplac

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=cnr_________::d2dd54790e927cdd9dbe1f510b62d924
http://www.cnr.it/prodotto/i/381444

Comment on: 'Borgia A., Mazzoldi A., Brunori C.A., Allocca C., Delcroix C., Micheli L., Vercellino A., Grieco, G., 2014. Volcanic spreading forcing and feedback in geothermal reservoir development,Amiata Volcano,Italia. J. Volc. Geoth. Res. 284, 16-31

Autor: Barazzuoli P.[1], Bertini G.[2], Brogi A.[3], Capezzuoli E.[4], Conticelli S.[5], Doveri M.[2], Ellero A.[2], Gianelli G. [2], La Felice S.[2], Liotta D.[3, Marroni M.[6], Manzella A.[2], Meccheri M.[1], Montanari D.[7], Pandeli E.[5], Principe C.[2], Ruggieri G.[2], Sbrana A.[6], Vaselli O.[5, Vezzoli L.[8

Publikováno v: Journal of volcanology and geothermal research 303 (2015): 1–6. doi:10.1016/j.jvolgeores.2015.07.004
info:cnr-pdr/source/autori:Barazzuoli P.[1], Bertini G.[2], Brogi A.[3], Capezzuoli E.[4], Conticelli S.[5], Doveri M.[2], Ellero A.[2], Gianelli G. [2], La Felice S.[2], Liotta D.[3,2], Marroni M.[6], Manzella A.[2], Meccheri M.[1], Montanari D.[7], Pandeli E.[5], Principe C.[2], Ruggieri G.[2], Sbrana A.[6], Vaselli O.[5,2], Vezzoli L.[8,2]/titolo:Comment on: "Borgia A., Mazzoldi A., Brunori C.A., Allocca C., Delcroix C., Micheli L., Vercellino A., Grieco, G., 2014. Volcanic spreading forcing and feedback in geothermal reservoir development,Amiata Volcano,Italia. J. Volc. Geoth. Res. 284, 16-31/doi:10.1016%2Fj.jvolgeores.2015.07.004/rivista:Journal of volcanology and geothermal research/anno:2015/pagina_da:1/pagina_a:6/intervallo_pagine:1–6/volume:303

Borgia et al. (2014) illustrated an active volcanic spreading model for the Amiata volcanic area (southern Tuscany, Italy). Although, at first glance, the model may appear appealing, this is not fully supported by the available data and the paper doe

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=cnr_________::1bc188ba886150402e588db9e4ee9626
https://publications.cnr.it/doc/334303