A tentative correlation between seismic activity and changes in the composition of thermal waters at Vulcano Island, Italy. (Articolo in rivista)

Type
Label
  • A tentative correlation between seismic activity and changes in the composition of thermal waters at Vulcano Island, Italy. (Articolo in rivista) (literal)
Anno
  • 1997-01-01T00:00:00+01:00 (literal)
Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#doi
  • 10.1016/S0375-6505(96)00049-1 (literal)
Alternative label
  • Bolognesi L. (1997)
    A tentative correlation between seismic activity and changes in the composition of thermal waters at Vulcano Island, Italy.
    in Geothermics; Pergamon-Elsevier Science Ltd., Oxford (Regno Unito)
    (literal)
Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#autori
  • Bolognesi L. (literal)
Pagina inizio
  • 379 (literal)
Pagina fine
  • 392 (literal)
Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#url
  • http://dx.doi.org/10.1016/S0375-6505(96)00049-1 (literal)
Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#numeroVolume
  • 26 (literal)
Rivista
Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#pagineTotali
  • 14 (literal)
Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#numeroFascicolo
  • 3 (literal)
Note
  • ISI Web of Science (WOS) (literal)
Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#affiliazioni
  • CNR - Istituto Internazionale per le Ricerche Geotermiche (literal)
Titolo
  • A tentative correlation between seismic activity and changes in the composition of thermal waters at Vulcano Island, Italy. (literal)
Abstract
  • On Vulcano Island, Italy, the thermal water in the shallow water well W2 is a mixture of reservoir water and shallow steam-heated groundwater of meteoric origin. In the period 1986-1988, the composition of the W2 water changed just before two sequences of tectonic earthquakes, from the almost pure reservoir component to the almost pure steam-heated meteoric component. After the seismic activity, the W2 water returned to its pre-earthquake reservoir composition. These changes in composition could be explained by the dilatancy-fluid diffusion model. According to this model, the observed variations in W2 water composition could be the consequence of stress build-up prior to the seismic events, and stress reduction afterwards. (literal)
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