Please use this identifier to cite or link to this item: http://hdl.handle.net/2122/7264
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dc.contributor.authorallCarlino, S.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione OV, Napoli, Italiaen
dc.contributor.authorallSomma, R.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione OV, Napoli, Italiaen
dc.contributor.authorallTroise, C.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione OV, Napoli, Italiaen
dc.contributor.authorallDe Natale, G.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione OV, Napoli, Italiaen
dc.date.accessioned2011-12-22T11:09:07Zen
dc.date.available2011-12-22T11:09:07Zen
dc.date.issued2012en
dc.identifier.urihttp://hdl.handle.net/2122/7264en
dc.description.abstractSince Roman time, the heat produced by Neapolitan volcanoes was an appeal for people living in and outside the area, for the fruition of the famous thermal baths. This very large area, which spans from Campi Flegrei and Ischia calderas to Somma-Vesuvius volcano, is characterized by high temperature at shallow depth and intense heat flow, and is yet utilized for the bathing and spa treatment industry, while only in the middle of the 20th century a tentative of geothermal exploitation for energy production was performed. Pioneering researches of geothermal resource were carried out in Campanian region since 1930, until 1985, during which a large amount of geological data were collected. In this paper, we make for the first time a review of the history of geothermal explorations in the active Campanian volcanic area. By the analysis of a great amount of literature data and technical reports we reconstruct the chronology and the main information of the drillings performed since 1930 by the SAFEN Company and successively in the framework of the ENEL-AGIP Joint Venture for geothermal exploration. The available data are utilized to correlate the temperatures measured within the deeper wells with the possible sources of geothermal heat in the shallow crust, down to about 8–10 km of depth. Finally, we assess the geothermal potential of the hottest areas, Ischia Island and Campi Flegrei, which have shown the best data and favorable physical conditions for a reliable, and cost-effective, exploitation for thermal and electric purposes.en
dc.description.sponsorshipEU-VIIFP GEISER Project (ENERGY:2009.2.4.1)en
dc.language.isoEnglishen
dc.publisher.nameELSEVIERen
dc.relation.ispartofRenewable and Sustainable Energy Reviewsen
dc.relation.ispartofseries1/16 (2012)en
dc.subjectCampi Flegreien
dc.subjectGeothermal potentialen
dc.subjectGeothermen
dc.subjectCampanian Volcanoesen
dc.subjectIschiaen
dc.subjectVesuviusen
dc.titleThe geothermal exploration of Campanian volcanoes: Historical review and future developmenten
dc.typearticleen
dc.description.statusPublisheden
dc.type.QualityControlPeer-revieweden
dc.description.pagenumber1004-1030en
dc.subject.INGV03. Hydrosphere::03.04. Chemical and biological::03.04.06. Hydrothermal systemsen
dc.identifier.doi10.1016/j.rser.2011.09.023en
dc.relation.references[1] Carlino S, Cubellis E, Delizia I, Luongo G. The history of Ischia harbour (Southern Italy). In: Viorel Badescu, Cathcart Richard B, editors. Macro-engineering seawater in/and unique environments. Arid lowlands and water bodies rehabilitation. Springer-Verlag; 2010., doi:10.1007/978-3-642-14779-1 2. [2] Carella R, Palmerini CG, Stefani GC, Verdini G. Geothermal activity in Italy: present status and prospects. In: Seminar on utilization of geothermal energy for electirc power production and space heating. 1984, 14–17 May. [3] AGIP. Geologia e geofisica del sistema geotermico dei Campi Flegrei, Technical report. Settore Esplor e Ric Geoterm-Metodol per l’Esplor Geotermica, San Donato Milanese Italy 1987;1–23. [4] ENEL. The Hystory of Larderello, Public Relations and Communications Dept., Ente Nazionale per l’Energia Elettrica; 1933. [5] Carrara E, Iacobucci F, Pinna E, Rapolla A. Gravity and magnetic survey of the campanian volcanic area, Southern Italy. Boll Geof Teor Appl 1973;XV 57:39–51. [6] Finetti I, Morelli C. Esplorazione di sismica a riflessione dei Golfi di Napoli e Pozzuoli. Boll Geof Teor Appl 1974;16:175–222. [7] Capaldi G, Civetta L, Gillot PY. Geochronology of Plio-Pleistocene volcanic rocks from southern Italy. Rend Soc Ital Miner Petrol 1985;40:25–44. [8] Fedi M, Rapolla A. The Campanian Volcanic area: analysis of the magnetic and gravimetric anomalies. Boll Soc Geol It 1987;106:793–805. [9] Rapolla A, Fedi M, Fiume MG. Crustal structure of Ischia–Phlegrean geothermal fields, near Naples, Italy, from gravity and aeromagnetic data. Geophys J 1989;97:409–19. [10] Acocella V, Faccenna C, Funiciello R, Rossetti F. Sand-box modelling of basement controlled transfer zones in extensional domains. Terranova 1999;11:149–56. [11] Patacca E, Sartori R, Scandone P. Tyrrhenia basin and Apenninic arcs: kinematic relation since late Tortonian times. Mem Soc Geol Ital 1990;45: 425–51. [12] Scandone R, 0 Giacomelli L, Speranza F. Persistent activity and violent strombolian eruptions at Vesuvius between 1631 and 1944. J Volcan Geoth Res 2007;170(3–4):167–80. [13] Della Vedova B, Bellani S, Pellis G, Squarci P. Deep temperatures and surface heat flow distribution. In: Vai GB, Martini IP, editors. Anatpmy of an Orogen: the Apennines and Adjacent Mediterranean basins. Kluwer Academic Publishers; 2001. p. 65–76. [14] Santacroce R, Somma-Vesuvius, Quaderni de La Ricerca Scientifica vol. 8, CNR, Roma 1987;114:p. 243. [15] Rolandi G, Bellucci F, Cortini M. A new model for the formation of the Somma Caldera. Mineral Petrol 2004;80:27–44. [16] D’Argenio B, Pescatore T, Scandone P. Schema Geologico dell’Appennino Meridionale (Campania e Lucania). Roma: Accademia Nazionale dei Lincei, q. 183, 1973 Atti del Convegno “Moderne vedute della geologia dell’Appennino”. [17] Ippolito F, D’Argenio B, Pescatore T, Scandone P. Structural–stratigraphic units and tectonic framework of southern Appennines. In: Squyres C, editor. Geology of Italy. Lybian Society of Earth Science. Libyan Arab Republic, 1975: 317–28. [18] Brocchini D, Principe C, Castradori D, Laurenzi MA, Gorla L. Quaternary evolution of the southern sector of the Campanian Plain and early Somma–Vesuvius activity, insights from the Trecase 1 well. Mineral Petrol 2001;73: 67–91. [19] Bruno P, Cippitelli G, Rapolla A. Seismic study of the Mesozoic carbonate basement around Mt. Somma–Vesuvius, Italy. J Volcanol Geotherm Res 1998;84:311–22. [20] Joron JL, Metrich N, Rosi M, Santocroce R, Sbrana A. Chemistry and petrography. In: Santacorce, R, editor. Somma–Vesuvius, Quad Ric Sci CNR, vol. 114. 1987. p. 105–74. [21] Sphera, FJ, De Vivo B, Ayuso RA, Belkin HE, editors. Special issue: Vesuvius. J Volcanol Geotherm Res 1998;82:1–247. [22] De Vivo B, Rolandi G. Mt. Somma–Vesuvius and volcanism of the Campanian Plain. Mineral Petrol 2001;73:233. [23] Somma R, Ayuso RA, De Vivo B, Rolandi G. Major, trace element and isotope geochemistry (Sr–Nd–Pb) of interplinian magmas from Mt. Somma–Vesuvius (southern Italy). Mineral Petrol 2001;73:121–43. [24] Scaillet B, Pichavant M, Cioni R. Upward migration of Vesuvius magma chamber over the past 20,000 years. Nature. doi:10.1038/nature07232. [25] De Natale G, Troise C, Trigila R, Dolfi D, Chiarabba C. Seismicity and 3D substructure at Somma–Vesuvius volcano: evidence for magma quenching. Earth Planet Sci Lett 2003;221:181–96. [26] Fedi M, Florio G, Rapolla A. 2.5D modelling of Somma–Vesuvius structure by aeromagnetic data. J Volcanol Geotherm Res 1998;82(1–4):239–47. [27] Marianelli P, Metrich N, Sbrana A. Shallow and deep reservoirs involved in magma supply of the 1944 eruption of Vesuvius. Bull Volcanol 1999;61:48–63. [28] Auger M, Gasparini P, Virieux J, Zollo A. Seismic evidence of an extended magmatic sill under Mt. Vesuvius. Science 2001;294:1510–2. [29] Zollo A, Gasparini P, Virieux J, le Meur H, De Natale G, Biella G, et al. Seismic evidence for a low-velocity zone in the upper crust beneath Mount Vesuvius. Science 1996;274:592–4. [30] Di Maio R, Mauriello P, Patella D, Petrillo Z, Piscitelli S, Siniscalchi A. Electric and electromagnetic outline of the Mt. Somma–Vesuvius structural setting. J Volcanol Geotherm Res 1998;82(1–4):219–38.[31] De Natale G, Troise C, Pingue F, De Gori P, Chiarabba C. Structure and dynamics of the Somma–Vesuvius volcanic complex. Mineral Petrol 2001;73:5–22. [32] Corrado G, Rapolla A. The gravity field of Italy: analysis of its spectral composition and delineation of a three-dimensional crustal model for central–southern Italy. Boll Geofis Teor Appl 1981;XXIII 89:17–29. [33] Ferrucci F, Gaudiosi G, Pino NA, Luongo G, Hirn A, Mirabile L. Seismic detection of a major Moho upheaval beneath the Campania volcanic area (Naples, Southern Italy). Geophys Res Lett 1989;16:1317–20. [34] Anderson H, Jackson J. The deep seismicity of the Tyrrhenian Sea. Geophys J R Astron Soc 1987;91:613–37. [35] Milano M, Vilardo G, Luongo G. Continental collision and basin opening in Southern Italy: a new plate subduction in the Tyrrhenian Sea? Tectonophysics 1994;230:249–64. [36] Rosi M, Sbrana A. Phlegrean fields. In: Rosi M, Sbrana A, editors. Phlegrean fields. Consig Naz Ric, Quadermi de la Ricerra Scientifica 1987;114:1–175. [37] Orsi G, Gallo G, Zanchi A. Simple-shearing block resurgence in caldera depressions. A model from Pantelleria and Ischia. J Volcanol Geotherm Res 1991;47:1–11. [38] Rolandi G, Bellucci F, Heizler MT, Belkin HE, De Vivo B. Tectonic controls on the genesis of ignimbrites from the Campanian Volcanic Zone, southern Italy. Mineral Petrol 2003;79:3–31. [39] Deino AL, Orsi G, de Vita S, Piochi M. The age of the Neapolitan Yellow Tuff caldera-forming eruption (Campi Flegrei caldera, Italy) assessed by 40Ar/39Ar dating method. J Volcanol Geotherm Res 2004;133:157–70. [40] Dvorak JJ, Mastrolorenzo G. The mechanism of recent vertical crustal movements in Campi Flegrei caldera, southern Italy. Geol Soc Am Spec Pap 1991;263:1–48. [41] Bellucci F, Woo J, CRJ, Rolandi G. The Campi Flegrei caldera: unrest mechanisms and hazards Geological Society, London, Special Publications 2006;269:141–57. [42] Morhange C, Bourciern M, Laborel J, Gialannella C, Goiran JP, Crimaco L, et al. New data on historical relative sea level movements in Pozzuoli Phlaegrean Fields, southern Italy. Phys Chem Earth 1999;A24:349–54. [43] Morhange C, Marriner N, Laborel J, Todesco Me, Oberlin C. Rapid sea-level movements and noneruptive crustal deformations in the Phlaegrean Fields caldera, Italy. Geology 2006;34(2):93–6. [44] Lirer L, Luongo G, Scandone R. On the volcanological evolution of Campi Flegrei. EOS Trans. AGU 68 1987:226–234. [45] De Natale G, Pingue F, Allard P, Zollo A. Geophysical and geochemical modelling of the Campi Flegrei caldera. J Volcanol Geotherm Res 1991;48:199–222. [46] Zollo A, Maercklin N, Vassallo M, Dello Iacono D, Virieux J, Gasparini P. Seismic reflections reveal a massive melt layer feeling Campi Flegrei caldera. Geophys Res Lett 2008;35:L12306, doi:10.1029/2008GL034242. [47] Berrino G, Corrado G, Luongo G, Toro B. Ground deformation and gravity changes accompanying the Pozzuoli uplift. Bull Volcanologique 1984;47:187–200. [48] Bianchi R, Coradini A, et al. Modelling of surface ground deformation in volcanic areas: the 1970–1972 and 1982–1984 crises of Campi Flegrei, Italy. J Geophys Res 1987;92:14139–50. [49] Quareni F. Finite element deformation of an elastic, nonuniform medium produced by a dilating or pressurised magma chamber. Geophys J Int 1990;101:243–9. [50] Bonafede M. Hot fluid migration: an efficient source of ground deformation; application to the 1982–1985 crisis at Campi Flegrei–Italy. J Volcanol Geotherm Res 1991;48:187–98. [51] De Natale G, Pingue F. Ground deformations in collapsed caldera structures. J Volcanol Geotherm Res 1993;57:19–38. [52] Trasatti E, Giunchi C, Bonafede M. Structural and rheological constraints on source depth and overpressure estimates at Campi Flegrei caldera, Italy. J Volcanol Geotherm Res 2005;144:105–18. [53] Gottsmann J, Rymer H, Berrino G. Unrest at the Campi Flegrei caldera (Italy): a critical evaluation of source parameters from geodetic data inversion. J Volcanol Geotherm Res 2006;150:132–45. [54] Battaglia M, Troise C, Obrizzo F, Pingue F, De Natale G. Evidence for fluid migration as source of deformation at Campi Flegrei caldera (Italy). Geophys Res Lett 2006;33, doi:10.1029/2005GL024904. [55] Amoruso A, Crescentini L, Berrino G. Simultaneous inversion of deformation and gravity changes in a horizontally layered halfspace: Evidence for magma intrusion during the 1982–1984 unrest at Campi Flegrei caldera (Italy). Earth Planet Sci Lett. doi:10.1016/j.epsl.2008.04.040. [56] Carlino S, Somma R. Eruptive versus non-eriptive behaviour of large calderas: the example of Campi Flegrei caldera (southern Italy). Bull Volcanol 2010, doi:10.1007/s00445-010-0370-y. [57] Troiano A, DiGiuseppe MG, Petrillo Z, Troise C, DeNatale G. Ground deformation at calderas driven by fluid injection: modelling unrest episodes at CampiFlegrei (Italy). doi:10.1111/j.1365-246X.2011.05149. [58] Vezzoli, L. Island of Ischia. Quaderni de La Ricerca Scientifica–CNR, 1988;114:p. 133. [59] Fusi N, Tibaldi A, Vezzoli L. Vulcanismo, risorgenza calderica e relazioni con la tettonica regionale nell’isola d’Ischia. Memorie della Società Geologica Italiana 1990;45:971–80. [60] Luongo G, Cubellis E, Di Vito, MA, Cascone E. L’isola d’Ischia: dinamica e struttura del M. Epomeo. In: Cinquanta Anni di Attività Didattica e Scientifica del Prof. F. Ippolito. Liguori, Naples 1995:427–36.[61] Acocella V, Funiciello R. The interaction between regional and local tectonics during resurgent doming: the case of the island of Ischia, Italy. J Volcanol Geotherm Res 1999;88:109–23. [62] Cubellis E, Del Gaudio C, Ferri M, Grimaldi M, Obrizzo F, Ricco C, et al. Gravity anomalies in the Campanian Plain (Southern Italy) and their volcano-tectonic implications. Acta Vulcanol 1991;1:57–62. [63] Tibaldi A, Vezzoli L. The space problem of caldera resurgence: an example from Ischia Island, Italy. Geol Rundsch 1998;87:53–66. [64] Tibaldi A, Vezzoli L. A new type of volcano flank failure: the resurgent caldera sector collapse, Ischia, Italy. Geophys Res Lett 2004;31:L14605, doi:10.1029/2004GL020419. [65] Carlino S, Cubellis E, Luongo G, Obrizzo F. On the mechanics of caldera resurgence of Ischia Island (southern Italy). In: Troise C, De Natale G, Kilburn CRJ, editors.) 2006. Mechanisms of Activity and Unrest at Large Calderas. Geological Society, London, Special Publications, 2006; 269:181–193. [66] Di Napoli R, Aiuppa A, Bellomo S, Brusca L, D’Alessandro W, Gagliano Candela E, et al. A model for Ischia hydrothermal system: evidences from the chemistry of thermal groundwaters. J Volcanol Geotherm Res 2009;186: 133–59. [67] Paoletti V, Di Maio R, Cella F, Florio G, Motschka K, Roberti N, et al. The Ischia volcanic island (Southern Italy): inferences from potential field data interpretation. J Volcanol Geotherm Res 2009;179(1–2):69–86. [68] Sbrana A, Fulignati P, Marianelli P, Boyce AJ, Cecchetti A. Exhumation of an active magmatic-hydrothermal system in a resurgent caldera environment: the example of Ischia (Italy). J Geol Soc London 2009;166:1016–73. [69] Lyell C. Principles of Geology, 3 vols. John Murray, London. Republished in 1990 by Univ of Chicago Press, Chicago, 1830 to 1833: 1399 pp. [70] Presti D, Troise C, De Natale G. Probabilistic location of seismic sequences in heterogeneous media. B-11 Seismol Soc Am 2004;94:2239–53. [71] Corrado G, Guerra I, Lo Bascio A, Luongo G, Rampoldi R. Inflation and microearthquake activity of phlegraean fields, Italy. Bull Volcanol 1976;40(3):169–88. [72] Berrino G. Gravity changes induced by heightmass variations at the Campi Flegrei caldera. J Volcanol Geotherm Res 1994;61:293–309. [73] De Natale G, Troise C, Pingue F, Mstrolorenzo G, Pappalardo L, Battaglia M, et al. The Campi Flegrei caldera: unrest mechanisms and hazards. In: Troise C, De Natale G, Kilburn CRJ, editors. Mechanisms of activity and unrest at large calderas. Geol Soc London Spec Pub. 2006;269:25–45. [74] Zamora M, Sartoris G, Chelini W. Laboratory measurements of ultrasonic wave velocities in rocks from the Campi Flegrei volcanic system and their relation to other field data. J Geophys Res 1994;99:13553–61. [75] Cubellis E, Ferri M, Luongo G, Obrizzo F. The roots of Mt. Vesuvius deduced from gravity anomalies. Mineral Petrol 2001;73:23–38. [76] Rabaute A, Yven B, CheliniW, Zamora M. Subsurface geophysics of Phlegrean Fields: new insights from downhole measurements. J Geophys Res;108:2171. doi:10.1029/20015B001436. [77] Judenherc S, Zollo A. The Bay of Naples (southern Italy): constraints on the volcanic structures inferred from dense seismic survey. J Geophys Res 2004;109:B10312, doi:10.1029/2003JB002876. [78] Troise C, De Natale G, Pingue F, Obrizzo F, De Martino P, Tammaro U, et al. Renewed ground uplift at Campi Flegrei caldera (Italy): new insight on magmatic processes and forecast. Geophys Res Lett 2007;34:L03301, doi:10.1029/2006GL028545. [79] Vinciguerra S, Trovato C, Meredith PG, Bensos PM, Troise C, De Natale G. Understanding the seismic velocity structure of Campi Flegrei caldera (Italy): from the laboratory to the field scale. Pure Appl Geophys 2006;163:2205–21. [80] Iasolino G. De’ rimedi naturali che sono nell’isola di Pithecusa oggi detta Ischia. Napoli; 1588. [81] Penta F. Temperature nel sottosuolo della regione Flegrea. Ann Geofis 1949;2:328–46. Penta 1949. [82] Barberi F, Cioppi D, Ghelardoni R, Nannini R, Sommaruga C, Verdini G. Integrated geothermal reconnaissance of the Somma-Vesuvius system. In: Commission of the European Communities. 2nd International Seminar. 1980. p. 141–53. [83] Chiodini G, Marini L, Russo M. Geochemical evidence for the existence of high-temperature hydrothermal brines at Vesuvio volcano, Italy. Geochim Cosmochim Acta 2001;65(13):2129–47. [84] Penta F, Conforto B. Risultati di sondaggi e di ricerche geominerarie nell’isola d’Ischia dal 1939 al 1943 nel campo di vapore, delle acque termali e delle forze endogene in generale. Ann Geofis 1951;4:159–91. [85] Cioppi D, Ghelardoni R, Panci G, Sommaruga C, Verdiani G. Demonstration project: evaluation of the Mofete high enthalpy reservoir (Phlegreans Fields). In: Commission of the European Communities, Second International Seminar–Palais des Congres. 1980. [86] Bruni P, Sbrana A, Silvano A. Risultati geologigi preliminary dell’esplorazione geotermica nell’area dei Campi Flegrei. Rend Soc Geol It 1981;4:231–6. [87] Balducci S, Vaselli M, Verdiani G. Exploration well in the Ottaviano Permit, Italy, Trecase 1, European Geothermal Update. In: 3rd International Seminar. 1983. p. 407–18. [88] Bruni P, Chelini W, Sbrana A, Verdiani G. Deep exploration of the S. Vito Area–Pozzuoli–Na S. Vito 1. In: Third International Seminar, European Geothermal Up date Munich 29 Nov-1 Dec. 1983. p. 390–406. [89] Carella R, Giglieliminetti M, Verdiano G. Attività dell’AGIP nel campo dell’energia geotermica in Italia. Convegno della Federelerrica, Padova 10 Aprile; 1986.[90] Dellea R, Morelli GC. Studi geochimici eseguiti su vari pozzi geotermici AGIP, Atti del Congresso S.I.M.P. Palermo, 17–22 Ottobre 1983. [91] Antrodicchia E, Cioni R, Chiodini G, Gagliardi R, Marini L. Geochemical temperatures of the thermal waters of Phlegraean Fields (Naples, Italy). In: Int. Symp. on Geothermal Energy. 1985. [92] Verdiani, G. Il punto sulla ricerca geotermica nell’area napoletana–Quale futuro per la geotermia ad Ischia? Convegno Casamicciola Terme 3–4 Maggio 1986. [93] ENEL. Inventario delle risorse geotermiche nazionali, Regione Campania allegato 2, schede dei pozzi provincial di Napoli, Pisa; 1987. [94] Fournier RO. The transition from hydrostatic to greater than hydrostatic fluid pressure in presently active continental hydrothermal systems in crystalline rocks. Geophys Res Lett 1991;18:955–8. [95] Fridleifsson IB. Status of geothermal energy amongst the world’s energy sources. Geothermics 2003;32(4–6):379–88. [96] Parancandola A. I fenomeni bradisismici del Serapeo di Pozzuoli, Napoli; 1947. [97] Carella R, Guglielminetti M. Multiple reservoirs in the Mofete Fields, Naples Italy, Ninth Workshop on Geothermal Resrvoir engineering, Stanford University, California, 13–15 Dec 1983. [98] Chelini W. Alcuni aspetti geologico-petrografici sul sistema geotermico Flegreo, rendiconti della Società Italiana di Mineralogia e Petrologia vol 1984;39:387–391. [99] Rittmann A. Geologie der Insel Ischia (Berlino). Zeitschrift für Vulkanologie 1930;VI:268. [100] Iovene F. Studio termico dell’Isola d’Ischia, Bollettino Società Naturalisti Napoli 1939:141–7. [101] Marini L, Franceschini F, Ghigliotti M, Guidi M, Merla A. Valutazione del Potenziale Geotermico Italiano. Ministero dell’Industria, del Commercio e dell’Artigianato. Inventario delle Risorse Geotermiche Nazionali, 1993: p. 104. [102] Nakada S, Uto K, Sakuma S, Eichelberger JC, Shimizu H. Scientific Results of Conduit Drilling in the Unzen Scientific Drilling Project (USDP). Scientific Drilling 2005;1:18–22. [103] De Natale G, Troise C, Trigila R, Dolfi D, Chiarabba C. Seismicity and 3D substructure at Somma-Vesuvius volcano: evidence for magma quenching. Earth Plan Sci Lett 2004;221:181–96. [104] Maino A, Tribalto G. Rilevamento gravimetrico di dettaglio dell’Isola d’Ischia. Boll Serv Geol Ital 92, 1971:109–23. [105] Nunziata C, Rapolla A. A gravity and magnetic study of the volcanic island of Ischia, Naples (Italy). J Volcanol Geotherm Res 1987;31:333–44. [106] Zollo A, Judenherc S, Auger E, D’Auria L, Virieux J, Capuano P, et al. Evidence for the buried rim of Campi Flegrei caldera from 3-D active seismic imaging. Geophys Res Lett 2002;30. DOI 10.1029/2003GL018173,2003. [107] Wohletz K, Civetta L, Orsi G. Thermal evolution of the Phlegreaean magmatic system. J Volcanol Geotherm Res 1999;91:381–414. [108] Turcotte DL, Schubert G. Geodynamics. Cambridge University Press; 2002. p. 456. [109] Corrado G, De Lorenzo S, Monelli F, Tramacere A, Zito G. Surface heat flow density at the Phlegrean Fields Caldera (Southern Italy). Geothermics 1998;27(4):469–84. [110] Schon JH. Physical properties of rocks. Elsevier; 2004, 583 pp. [111] Aster RC, Mayer RP. Three-dimensional velocity structure and hypocenter distribution in the Campi Flegrei caldera, Italy. Tectonophysics 1988;149(3–4):195–218.[112] Hill D. Temperatures at the base of the seismogenetic crust beneath Long Valley caldera, California, and Phlegrean Fields caldera, Italy. In: Gasparini P, Scarpa R, Aki K, editors. Volcanic Seismology IAVCEI Proceedings in Volcanology 3. Germany: Springer; 1992. p. 432–61. [113] Carlino S, Cubellis E, Maturano A. The catastrophic 1883 earthquake at the island of Ischia (southern Italy): macroseismic data and the role of geological conditions. Nat Hazards 2009, doi:10.1007/s11069-009-9367-2. [114] Carslaw HS, Jaeger JC. Conduction of heat in solids. 2nd ed. Oxford: Clarendon Press; 1959. [115] Bear J. Dynamic of fluids in porous media. American: Elsevier Publisher Company; 1972, 757 pp. [116] Goguel R. Thermal water transport of some major rock constituents at Wairakei. N Z J Sci 1976;19:359–68. [117] Fyfe WS, Price NJ, Thompson AB. Fluids in the earth’s crust: their significance in metamorphic, tectonic, and chemical transport processes. Elsevier Scientific Pub. Co.; 1978, 383 pp. [118] Hurwitz S, Christiansen Lizet B, Hsieh PA. Hydrothermal fluid flow and deformation in large calderas: inferences from numerical simulation. J Geoph Res 2007, doi:10.1029/2006JB004689. [119] Civetta L, Gallo G, Orsi G. Sr and Nd isotope and trace element constraints on the chemical evolution of the magmatic system of Ischia (Italy) in the last 55.000 ka. J Volcanol Geotherm Res 1991;46:213–320. [120] Gaeta FS, De Natale G, et al. Genesis and evolution of unrest episodes at Campi Flegrei caldera: the role of thermal fluid dynamical processes in the geothermal system. J Geophys Res 1998;103:20921–33. [121] Orsi G, D’Antonio M, de Vita S, Gallo G. The Neapolitan Yellow Tuff, a large-magnitude trachytic phreatoplinian eruption: Eruptive dynamics, magma withdrawal and caldera collapse. J Volcanol Geotherm Res 1992;53: 275–87. [122] Muffler P, Cataldi R. Methods for regional assessment of geothermal resources. Geothermics 1978;7:53–89. [123] Grant MA, Donaldson IG. Geothermal reservoir engineering. Camarillo, CA: Geothermal World Info Center; 1983, 376 pp. [124] Doveri M, Lelli M, Luigi Marini L, Raco B. Revision, calibration, and application of the volume method to evaluate the geothermal potential of some recent volcanic areas of Latium, Italy. Geothermics 2010;39(3):260–9. [125] Armstead HCH, Tester JW. Heat mining. London: E. & F. N. Spon Ltd.; 1978. [126] Smith R. Unpubblished Technical Report, UCL; 2006. [127] Panichi C, Bolognesi L, Ghiara MR, Noto P, Stanzione D. Geothermal assessment of the island of Ischia (southern Italy) from isotopic and chemical composition of the delivered fluids. J Volcanol Geotherm Res 1992;49:329–48. [128] Bono P. Valutazione preliminare del potenziale geotermico della regione laziale. Geol Rom 1981:2. [129] Chiodini G, Frondini C, Cardellini Granieri D, Marini L, Ventura G. CO2 degassing and energy release at Solfatara volcano, Campi Flegrei, Italy. J Geophys Res 2001;106(B8), 16,213–16,221. [130] Caliro S, Chiodini G, Moretti R, Avino R, Granieria D, Russo M, et al. The origin of the fumaroles of La Solfatara (Campi Flegrei, South Italy). Geochim Cosmochim Acta 2007;71(12):3040–55. [131] De Pippo R. Geothermal power plants. Elsevier; 2005. p. 493.en
dc.description.obiettivoSpecifico3.6. Fisica del vulcanismoen
dc.description.journalTypeJCR Journalen
dc.description.fulltextreserveden
dc.contributor.authorCarlino, S.en
dc.contributor.authorSomma, R.en
dc.contributor.authorTroise, C.en
dc.contributor.authorDe Natale, G.en
dc.contributor.departmentIstituto Nazionale di Geofisica e Vulcanologia, Sezione OV, Napoli, Italiaen
dc.contributor.departmentIstituto Nazionale di Geofisica e Vulcanologia, Sezione OV, Napoli, Italiaen
dc.contributor.departmentIstituto Nazionale di Geofisica e Vulcanologia, Sezione OV, Napoli, Italiaen
dc.contributor.departmentIstituto Nazionale di Geofisica e Vulcanologia, Sezione OV, Napoli, Italiaen
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 OV, Napoli, Italia-
crisitem.author.deptIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione OV, Napoli, Italia-
crisitem.author.deptIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione OV, Napoli, Italia-
crisitem.author.deptIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione OV, Napoli, Italia-
crisitem.author.orcid0000-0002-3924-3881-
crisitem.author.orcid0000-0002-2227-6054-
crisitem.author.orcid0000-0001-6555-5777-
crisitem.author.orcid0000-0001-8391-2846-
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.author.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
crisitem.classification.parent03. Hydrosphere-
crisitem.department.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
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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