Please use this identifier to cite or link to this item:
http://hdl.handle.net/2122/10474
DC Field | Value | Language |
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dc.contributor.authorall | Saroli, M.; Università degli studi di Cassino e del Lazio meridionale | en |
dc.contributor.authorall | Lancia, M.; Università degli studi di Cassino e del Lazio meridionale | en |
dc.contributor.authorall | Albano, M.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione CNT, Roma, Italia | en |
dc.contributor.authorall | Casale, A.; Università degli studi di Cassino e del Lazio meridionale | en |
dc.contributor.authorall | Giovinco, G.; Università degli studi di Cassino e del Lazio meridionale | en |
dc.contributor.authorall | Petitta, M.; DST-Dipartimento di Scienze della Terra, Sapienza Università di Roma | en |
dc.contributor.authorall | Zarlenga, F.; Unità Tecnica per le Fonti di Enertgia Rinnovabili – ENEA | en |
dc.contributor.authorall | dell'Isola, M.; Università degli studi di Cassino e del Lazio meridionale | en |
dc.date.accessioned | 2017-03-20T09:28:43Z | en |
dc.date.available | 2017-03-20T09:28:43Z | en |
dc.date.issued | 2017-03-17 | en |
dc.identifier.uri | http://hdl.handle.net/2122/10474 | en |
dc.description.abstract | A hydrogeological conceptual model has been de- veloped that describes the hydrothermal system of Suio Terme (central Italy). The studied area is located along the peri- Tyrrhenian zone of the central Apennines, between the Mesozoic and Cenozoic carbonate platform sequences of the Aurunci Mountains and the volcanic sequences of the Roccamonfina. A multi-disciplinary approach was followed, using newhydrogeological surveys, the interpretation of strat- igraphic logs of boreholes and water wells, and geophysical data—seismic sections, shear-wave velocity (Vs) crustal mod- el and gravimetric model. The collected information allowed for construction of a conceptual hydrogeological model and characterization of the hydrothermal system. The Suio hydro- thermal system is strongly influenced by the Eastern Aurunci hydrostructure. Along the southeastern side, the top of the hydrostructure sinks to −1,000 m relative to sea level via a series of normal faults which give origin to the Garigliano graben. Geological and hydrogeological data strongly suggest the propagation and mixing of hot fluids, with cold waters coming from the shallow karst circuit. The aquitard distribution, the normal tectonic displacements and the frac- turing of the karst hydrostructure strongly influence the hy- drothermal basin. Carbon dioxide and other gasses play a key role in the whole circuit, facilitating the development of the hydrothermal system. The current level of knowledge sug- gests that the origin of the Suio hydrothermalism is the result of interaction between the carbonate reservoir of the Eastern Aurunci Mountains and the hot and deep crust of this peri- Tyrrhenian sector, where the Roccamonfina volcano repre- sents | en |
dc.language.iso | English | en |
dc.publisher.name | Springer-Verlag Germany | en |
dc.relation.ispartof | Hydrogeology Journal | en |
dc.relation.ispartofseries | 6/25 (2017) | en |
dc.subject | Karst | en |
dc.subject | Conceptual model | en |
dc.subject | Italy | en |
dc.subject | Thermal conditions | en |
dc.subject | Hydrogeological | en |
dc.subject | Idrostructure | en |
dc.subject | Hydrotermal | en |
dc.title | A hydrogeological conceptual model of the Suio hydrothermal area (central Italy) | en |
dc.type | article | en |
dc.description.status | Published | en |
dc.description.pagenumber | 1811–1832 | en |
dc.subject.INGV | 03. Hydrosphere::03.02. Hydrology::03.02.02. Hydrological processes: interaction, transport, dynamics | en |
dc.subject.INGV | 03. Hydrosphere::03.02. Hydrology::03.02.03. Groundwater processes | en |
dc.identifier.doi | 10.1007/s10040-017-1549-5 | en |
dc.description.obiettivoSpecifico | 7A. Geofisica per il monitoraggio ambientale e geologia medica | en |
dc.description.journalType | JCR Journal | en |
dc.description.fulltext | restricted | en |
dc.relation.issn | 1431-2174 | en |
dc.relation.eissn | 1435-0157 | en |
dc.contributor.author | Saroli, M. | en |
dc.contributor.author | Lancia, M. | en |
dc.contributor.author | Albano, M. | en |
dc.contributor.author | Casale, A. | en |
dc.contributor.author | Giovinco, G. | en |
dc.contributor.author | Petitta, M. | en |
dc.contributor.author | Zarlenga, F. | en |
dc.contributor.author | dell'Isola, M. | en |
dc.contributor.department | Università degli studi di Cassino e del Lazio meridionale | en |
dc.contributor.department | Università degli studi di Cassino e del Lazio meridionale | en |
dc.contributor.department | Istituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione ONT, Roma, Italia | en |
dc.contributor.department | Università degli studi di Cassino e del Lazio meridionale | en |
dc.contributor.department | Università degli studi di Cassino e del Lazio meridionale | en |
dc.contributor.department | DST-Dipartimento di Scienze della Terra, Sapienza Università di Roma | en |
dc.contributor.department | Unità Tecnica per le Fonti di Enertgia Rinnovabili – ENEA | en |
dc.contributor.department | Università degli studi di Cassino e del Lazio meridionale | en |
item.openairetype | article | - |
item.cerifentitytype | Publications | - |
item.languageiso639-1 | en | - |
item.grantfulltext | restricted | - |
item.openairecristype | http://purl.org/coar/resource_type/c_18cf | - |
item.fulltext | With Fulltext | - |
crisitem.author.dept | University of Cassino | - |
crisitem.author.dept | Università degli Studi di Cassino e del Lazio Meridionale | - |
crisitem.author.dept | Istituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione ONT, Roma, Italia | - |
crisitem.author.dept | Department of Civil and Mechanical Engineering, University of Cassino and southern Lazio | - |
crisitem.author.dept | Department of Civil and Mechanical Engineering, University of Cassino and southern Lazio | - |
crisitem.author.dept | Unità Tecnica per le Fonti di Enertgia Rinnovabili – ENEA | - |
crisitem.author.dept | Department of Civil and Mechanical Engineering, University of Cassino and southern Lazio | - |
crisitem.author.orcid | 0000-0001-9499-3960 | - |
crisitem.author.orcid | 0000-0002-8703-6174 | - |
crisitem.author.orcid | 0000-0003-2772-2401 | - |
crisitem.author.orcid | 0000-0001-7559-7559 | - |
crisitem.author.orcid | 0000-0001-6779-5774 | - |
crisitem.author.orcid | 0000-0003-1137-6137 | - |
crisitem.author.orcid | 0000-0002-7104-740X | - |
crisitem.author.orcid | 0000-0001-7976-5484 | - |
crisitem.author.parentorg | Istituto Nazionale di Geofisica e Vulcanologia | - |
crisitem.classification.parent | 03. Hydrosphere | - |
crisitem.classification.parent | 03. Hydrosphere | - |
crisitem.department.parentorg | Istituto Nazionale di Geofisica e Vulcanologia | - |
Appears in Collections: | Article published / in press |
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Saroli et al. - 2017 - A hydrogeological conceptual model of the Suio hydrothermal area (central Italy).pdf | Main article | 9.45 MB | Adobe PDF |
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