Bibliographies thématiques / Somma-Vesuvio

Littérature scientifique sur le sujet « Somma-Vesuvio »

Auteur : Grafiati

Publié le 10 mars 2023

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Articles de revues sur le sujet "Somma-Vesuvio"

Alberico, I., P. Petrosino et L. Lirer. « Volcanic hazard and risk assessment in a multi-source volcanic area : the example of Napoli city (Southern Italy) ». Natural Hazards and Earth System Sciences 11, n^o 4 (7 avril 2011) : 1057–70. http://dx.doi.org/10.5194/nhess-11-1057-2011.

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Abstract. The possible emplacement of pyroclastic fall and flow products from Campi Flegrei and Somma-Vesuvio represents a threat for the population living in Napoli city. For this area, the volcanic hazard was always partially investigated to define the hazard related to the Campi Flegrei or to the Somma-Vesuvio activity one at a time. A new volcanic hazard and risk assessment, at the municipality scale, as a vital tool for decision-making about territorial management and future planning, is presented here. In order to assess the hazard related to the explosive activity of both sources, we integrated the results of field studies and numerical simulations, to evaluate the future possibility for Napoli to be hit by the products of an explosive eruption. This is defined for the Somma Vesuvio central volcano through the sum of "field frequency" based on the thickness and distribution of past deposits (Lirer et al., 2001), and for the Campi Flegrei volcanic field by suitably processing simulated events based on numerical modelling (Alberico et al., 2002; Costa et al., 2009). Aiming at volcanic risk assessment, the hazard areas were joined with the exposure map, considered for our purposes as the economical value of artefacts exposed to hazard. We defined four risk classes, and argued that the medium and low-very low risk classes have the largest extent in Napoli municipality, whereas only few zones located in the eastern part of the city and in the westernmost coastal area show a high risk, owing to the correspondence of high economical value and high hazard.

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Berrino, Giovanna, Ugo Coppa, Giuseppe De Natale et Folco Pingue. « Recent geophysical investigation at Somma-Vesuvio volcanic complex ». Journal of Volcanology and Geothermal Research 58, n^o 1-4 (novembre 1993) : 239–62. http://dx.doi.org/10.1016/0377-0273(93)90111-4.

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Balassone, G., A. Beran et Karl Lueger-Ring. « Variable water content of nepheline from Somma-Vesuvio, Italy ». Mineralogy and Petrology 52, n^o 1-2 (1995) : 75–83. http://dx.doi.org/10.1007/bf01163127.

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Ballirano, Paolo, Adriana Maras, Peter R. Buseck, Su Wang et Ann M. Yates. « Improved powder X-ray data for cancrinites I : Afghanite ». Powder Diffraction 9, n^o 1 (mars 1994) : 68–73. http://dx.doi.org/10.1017/s0885715600019722.

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Afghanite is a feldspathoid of the cancrinite-group: It is hexagonal, space group P63mc. The afghanite sample was found in the M. Somma-Vesuvio volcanic complex (Italy) and was previously described as davyne: Calculated cell parameters are a = 12.7997(4) Å, c = 21.4062(11) Å; the volume is 3037.2(2) Å3. The strongest lines are: 3.694(100), 3.647(56), 4.826(30), 2.678(25), 2.134(18), 3.999(12), 2.750(12), and 2.771(10). The new data provide quantitative measurement of intensities, an increased number of indexed peaks, and a different empirical formula with respect to the PDF 20-1086.

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Lirer, Lucio, Paola Petrosino, Ines Alberico et Immacolata Postiglione. « Long-term volcanic hazard forecasts based on Somma-Vesuvio past eruptive activity ». Bulletin of Volcanology 63, n^o 1 (8 mai 2001) : 45–60. http://dx.doi.org/10.1007/s004450000121.

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PORRECA, M., V. ACOCELLA, E. MASSIMI, M. MATTEI, R. FUNICIELLO et A. DEBENEDETTI. « Geometric and kinematic features of the dike complex at Mt. Somma, Vesuvio (Italy) ». Earth and Planetary Science Letters 245, n^o 1-2 (15 mai 2006) : 389–407. http://dx.doi.org/10.1016/j.epsl.2006.02.027.

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Donatella, De Rita, Dolfi Daniela et Cimarelli Corrado. « Occurrence of Somma-Vesuvio fine ashes in the tephrostratigraphic record of Panarea, Aeolian Islands ». Journal of Volcanology and Geothermal Research 177, n^o 1 (octobre 2008) : 197–207. http://dx.doi.org/10.1016/j.jvolgeores.2007.11.007.

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Caliro, S., G. Chiodini, R. Avino, C. Cardellini et F. Frondini. « Volcanic degassing at Somma–Vesuvio (Italy) inferred by chemical and isotopic signatures of groundwater ». Applied Geochemistry 20, n^o 6 (juin 2005) : 1060–76. http://dx.doi.org/10.1016/j.apgeochem.2005.02.002.

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Chukanov, Nikita V., Natalia V. Zubkova, Igor V. Pekov, Lyudmila V. Olysych, Elena Bonaccorsi et Dmitry YU Pushcharovsky. « Balliranoite, (Na,K)6Ca2(Si6Al6O24)Cl2(CO3), a new cancrinite-group mineral from Monte Somma Vesuvio volcanic complex, Italy ». European Journal of Mineralogy 22, n^o 1 (18 mars 2010) : 113–19. http://dx.doi.org/10.1127/0935-1221/2010/0022-1983.

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Rolandi, G., S. Maraffi, P. Petrosino et L. Lirer. « The Ottaviano eruption of Somma-Vesuvio (8000 y B.P.) : a magmatic alternating fall and flow-forming eruption ». Journal of Volcanology and Geothermal Research 58, n^o 1-4 (novembre 1993) : 43–65. http://dx.doi.org/10.1016/0377-0273(93)90101-v.

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Thèses sur le sujet "Somma-Vesuvio"

TADINI, ALESSANDRO. « Vent Opening Probability map and Pyroclastic Density Currents hazard assessment at Somma-Vesuvio through a multidisciplinary approach based on physical volcanology and numerical modeling ». Doctoral thesis, 2017. http://hdl.handle.net/2158/1079381.

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Il progetto di dottorato al termine del triennio ha permesso di raggiungere i seguenti obiettivi: a) costituzione di un database comprendente i dati vulcanologici più significativi per quanto riguarda lo sviluppo di una mappa di probabilità di apertura bocche all’interno della caldera del Somma-Vesuvio (SV); b) creazione di mappe di densità di probabilità per ogni dataset vulcanologico individuato in a) e combinazione lineare di tali mappe, opportunamente pesate tramite il giudizio degli esperti, per ottenere una prima mappa di probabilità apertura bocche con specifico riferimento al vulcanismo esplosivo; c) studio di terreno e di laboratorio di depositi selezionati di colate piroclastiche del SV per meglio definire le granulometrie iniziali dei flussi piroclastici, le aree invase dalle correnti e i volumi emessi; d) validazione di modelli fisici semplificati e simulazione numerica della formazione e propagazione dei flussi piroclastici utilizzando i nuovi parametri definiti in c), e) stima della pericolosità delle colate piroclastiche in caso di riattivazione del SV attraverso la creazione di una prima mappa probabilistica preliminare di invasione da flussi piroclastici. The PhD project, at the end of the 3 years, has allowed the achievement of the following objectives: a) the implementation of a Geo-Database which includes volcanological/structural data (where epistemic uncertainty has been quantified) useful for the development of a vent opening probability map within the present outline of the Somma-Vesuvio (SV) caldera; b) the definition of Probability Density Maps for each of the dataset defined in a) and the linear combination of such maps, with different weights defined after Structured Expert Judgement (SEJ) procedures, in order to obtain a first vent opening probability map with specific focus on explosive volcanism; c) field and laboratory analyses of selected PDC deposits in order to better define Total-Grain Size Distributions (TGSD), inundation areas and the volumes of eruptive units; d) the validation of simplified physical models and the numerical modeling of the formation and propagation of PDCs using as input parameters field data defined in c); e) PDC hazard assessment in case of a reactivation of SV through the implementation of a preliminary PDC probability invasion map for a specific scenario.

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Chapitres de livres sur le sujet "Somma-Vesuvio"

Bisson, Marina, Alessandro Tadini, Roberto Gianardi et Andrea Angioletti. « Morphological Evolution of Somma-Vesuvio During the Last Century : Integration Between Historical Maps and Airborne LiDAR Survey ». Dans R3 in Geomatics : Research, Results and Review, 311–20. Cham : Springer International Publishing, 2020. http://dx.doi.org/10.1007/978-3-030-62800-0_24.

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Albore Livadie, Claude, Guido D’Alessio, Giuseppe Mastrolorenzo et Giuseppe Rolandi. « Le eruzioni del Somma-Vesuvio in epoca protostorica ». Dans Tremblements de terre, éruptions volcaniques et vie des hommes dans la Campanie antique, 55–66. Publications du Centre Jean Bérard, 1986. http://dx.doi.org/10.4000/books.pcjb.2401.

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Rosi, Mauro, et Roberto Santacroce. « L’attività del Somma-Vesuvio precedente l’eruzione del 1631 : dati stratigrafici e vulcanologici ». Dans Tremblements de terre, éruptions volcaniques et vie des hommes dans la Campanie antique, 15–33. Publications du Centre Jean Bérard, 1986. http://dx.doi.org/10.4000/books.pcjb.2386.

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