Please use this identifier to cite or link to this item: http://hdl.handle.net/2122/5094
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dc.contributor.authorallItaliano, F.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione Palermo, Palermo, Italiaen
dc.contributor.authorallCaracausi, A.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione Palermo, Palermo, Italiaen
dc.contributor.authorallFavara, R.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione Palermo, Palermo, Italiaen
dc.contributor.authorallMartinelli, G.; ARPA Emilia Romagnaen
dc.contributor.authorallInnocenzi, P.; VUS-Folignoen
dc.date.accessioned2009-06-24T06:27:50Zen
dc.date.available2009-06-24T06:27:50Zen
dc.date.issued2005-10en
dc.identifier.urihttp://hdl.handle.net/2122/5094en
dc.description.abstractThe geochemical monitoring carried out on fluids released in the Central Apennines (Umbria region) evidenced seismically-induced modifications of the physic-chemical parameters in all the released fluids, including some cold waters circulating in certain carbonate rocks that are exploited for drinking purposes. The results allowed us to recognize the presence of components of diverse origin that changed the chemical composition of the water. These components, potentially dangerous for human consumption, can be considered as being “secondary effects” on local aquifers, induced by crustal deformation. We would also stress the relationship between the circulating fluids and active tectonic structures, as we detected modifications in some springs that were apparently not located anywhere near the local faults. The temporal variations in the geochemical features of the investigated cold waters are related to the local faulting activity that occurs during seismogenesis. The geochemical monitoring that provided information on fault movements during the seismic crisis, is also able to give us information regarding faulting activity in its earlier stages.en
dc.language.isoEnglishen
dc.publisher.nameChinese Geoscience Unionen
dc.relation.ispartofTAO -Terrestrial, Atmospheric and Oceanic sciencesen
dc.relation.ispartofseries4/16 (2005)en
dc.subjectcold watersen
dc.subjectearthquakesen
dc.titleGeochemical Monitoring of Cold Waters during Seismicity: Implications for Earthquake-induced Modification in Shallow Aquifersen
dc.typearticleen
dc.description.statusPublisheden
dc.type.QualityControlPeer-revieweden
dc.description.pagenumber709-729en
dc.subject.INGV04. Solid Earth::04.04. Geology::04.04.12. Fluid Geochemistryen
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Innocenzi, F. Italiano, and G. Martinelli, 2002: Variazioni geochimiche in acque sotterranee fredde dell’Umbria connesse con la sequenza sismica del 1997-1998. Acque Sotterranee, 78, 23-33. (in Italian) Boncio, P., F. Brozzetti, F. Ponziani, M. Barchi, G. La Vecchia, and G. Pialli, 1998: Seismicity and extensional tectonics in the Northern Umbria-Marche Apennines. Mem. Soc. Geol. It., 52, 539-555. Castello B., G. Selvaggi, C. Chiarabba, and A. Amato, 2005: CSI Catalogo della sismicità italiana 1981-2002, versione 1.0. INGV-CNT, Roma. http://www.ingv.it/CSI/ Caracausi, A., F. Italiano, G. Martinelli, A. Paonita, and A. Rizzo, 2005: Long-term geochemical monitoring and extensive/compressive phenomena: case study of the Umbria region(central Apennines, Italy). Annals of Geophysics, 48, 43-53. Chiodini, G., S. Giaquinto, and A. R. Zanzari, 1982: Relazione tra il chimismo delle sorgenti Umbre e le caratteristiche litologiche degli acquiferi. 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Tectonophysics, 304, 1-24. Zanzari, A. R., A. Martinelli, R. Cioni, M. Guidi, B. Raco, A. Scozzari, F. Quattrocchi, G.Galli, and C. Mancini, 2001: Discrete and continuous monitoring of groundwaters in the seismic area of the Umbria Region (Italy). WRI 2001, Cidu (Ed.), 1, 119-122.en
dc.description.obiettivoSpecifico3.2. Tettonica attivaen
dc.description.journalTypeN/A or not JCRen
dc.description.fulltextreserveden
dc.contributor.authorItaliano, F.en
dc.contributor.authorCaracausi, A.en
dc.contributor.authorFavara, R.en
dc.contributor.authorMartinelli, G.en
dc.contributor.authorInnocenzi, P.en
dc.contributor.departmentIstituto Nazionale di Geofisica e Vulcanologia, Sezione Palermo, Palermo, Italiaen
dc.contributor.departmentIstituto Nazionale di Geofisica e Vulcanologia, Sezione Palermo, Palermo, Italiaen
dc.contributor.departmentIstituto Nazionale di Geofisica e Vulcanologia, Sezione Palermo, Palermo, Italiaen
dc.contributor.departmentARPA Emilia Romagnaen
dc.contributor.departmentVUS-Folignoen
item.openairetypearticle-
item.cerifentitytypePublications-
item.languageiso639-1en-
item.grantfulltextrestricted-
item.openairecristypehttp://purl.org/coar/resource_type/c_18cf-
item.fulltextWith Fulltext-
crisitem.author.deptIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione Palermo, Palermo, Italia-
crisitem.author.deptIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione Palermo, Palermo, Italia-
crisitem.author.deptIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione Palermo, Palermo, Italia-
crisitem.author.deptARPA Emilia-Romagna-
crisitem.author.deptVUS-Foligno-
crisitem.author.orcid0000-0002-9465-6398-
crisitem.author.orcid0000-0003-2510-2890-
crisitem.author.orcid0000-0003-4588-2935-
crisitem.author.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
crisitem.author.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
crisitem.author.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
crisitem.classification.parent04. Solid Earth-
crisitem.department.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
crisitem.department.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
crisitem.department.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
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