Quantitative model for magma degassing and ground deformation (bradyseism) at Campi Flegrei, Italy: Implication for future eruptions (Articolo in rivista)

Type

• Prodotto della ricerca (Classe)
• Articolo in rivista (Classe)

Label

• Quantitative model for magma degassing and ground deformation (bradyseism) at Campi Flegrei, Italy: Implication for future eruptions (Articolo in rivista) (literal)

Anno

• 2007-01-01T00:00:00+01:00 (literal)

Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#doi

• 10.1130/G23653A.1 (literal)

Alternative label

• Bodnar R.J.; Cannatelli C.; De Vivo B.; Lima A.; Belkin H. E.; Milia A. (2007)
  Quantitative model for magma degassing and ground deformation (bradyseism) at Campi Flegrei, Italy: Implication for future eruptions
  in Geology (Boulder Colo.)
  (literal)

Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#autori

• Bodnar R.J.; Cannatelli C.; De Vivo B.; Lima A.; Belkin H. E.; Milia A. (literal)

Pagina inizio

• 791 (literal)

Pagina fine

• 794 (literal)

Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#numeroVolume

• 35/9 (literal)

Rivista

• Geology (Rivista)

Note

• Scopus (literal)
• ISI Web of Science (WOS) (literal)
• Google Scholar (literal)

Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#affiliazioni

• Dept of Geosciences, Virginia Polytechnic Institute and State University, 4044 Derring Hall, Blacksburg, Virginia 24061, USA Dip. di Scienze della Terra, Università di Napoli \"Federico II\", via Mezzocannone 8, 80138 Napoli U.S. Geological Survey,956 National Center, Reston, Virginia 20192, USA IAMC, CNR, Calata Porta di Massa, Porto di Napoli 80133 Italy (literal)

Titolo

• Quantitative model for magma degassing and ground deformation (bradyseism) at Campi Flegrei, Italy: Implication for future eruptions (literal)

Abstract

• Campi Flegrei (Phlegrean Fields) is an active volcanic center near Naples, Italy. Numerous eruptions have occurred here during the Quaternary, and repeated episodes of slow vertical ground movement (bradyseism) have been documented since Roman times. Here, we present a quantitative model that relates deformation episodes to magma degassing and fracturing at the brittle-ductile transition in a magmatic-hydrothermal environment. The model is consistent with fi eld and laboratory observations and predicts that uplift between 1982 and 1984 was associated with crystallization of ~0.83 km3 of H2O-saturated magma at 6 km depth. During crystallization, ~6.2 ~ 1010 kg of H2O and 7.5 ~ 108 kg of CO2 exsolved from the magma and generated ~7 ~ 1015 J of mechanical (Pƒ¢V) energy to drive the observed uplift. For comparison, ~1017 J of thermal energy was released during the 18 May 1980 lateral blast at Mount St. Helens. (literal)

Prodotto di

• Assetto geologico di siti mediterranei ed oceanici e rischi connessi nelle aree costiere (TA.P01.011.001) (Modulo)
• Institute for coastal marine environment (IAMC) (Istituto)

Autore CNR

• ALFONSA MILIA (Unità di personale interno)

Insieme di parole chiave

• Keywords of "Quantitative model for magma degassing and ground deformation (bradyseism) at Campi Flegrei, Italy: Implication for future eruptions" (Insieme di parole chiave)

Incoming links:

Prodotto

• Institute for coastal marine environment (IAMC) (Istituto)
• Assetto geologico di siti mediterranei ed oceanici e rischi connessi nelle aree costiere (TA.P01.011.001) (Modulo)

Autore CNR di

• ALFONSA MILIA (Unità di personale interno)

Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#rivistaDi

• Geology (Rivista)

Insieme di parole chiave di

• Keywords of "Quantitative model for magma degassing and ground deformation (bradyseism) at Campi Flegrei, Italy: Implication for future eruptions" (Insieme di parole chiave)