Please use this identifier to cite or link to this item:
http://hdl.handle.net/2122/430| DC Field | Value | Language |
|---|---|---|
| dc.contributor.authorall | Civetta, L.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione OV, Napoli, Italia | en |
| dc.contributor.authorall | D'Antonio, M.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione OV, Napoli, Italia | en |
| dc.contributor.authorall | de Lorenzo, S.; Dip. Geologia e Geofisica, University of Bari, Bari | en |
| dc.contributor.authorall | Di Renzo, V.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione OV, Napoli, Italia | en |
| dc.contributor.authorall | Gasparini, P.; Dip. Scienze Fisiche, Università Federico II, Napoli | en |
| dc.date.accessioned | 2005-09-28T09:53:23Z | en |
| dc.date.available | 2005-09-28T09:53:23Z | en |
| dc.date.issued | 2004 | en |
| dc.identifier.uri | http://hdl.handle.net/2122/430 | en |
| dc.description.abstract | A review of available and new isotopic data on rocks from Mt. Vesuvius together with geophysical and mineralogical data allow us to define a ‘deep’ complex magmatic reservoir where mantle-derived magmas arrive, stagnate and differentiate, and to constrain a thermal model, which describes the history and present state of the reservoir and its surrounding rocks. The top of the reservoir is located at about 8 km depth, and it extends discontinuously down to 20 km depth. The reservoir is hosted in densely fractured continental crustal rocks, where magmas and crust can interact, and, according to thermal modeling results, has been fed more than once in the last 400 ka. The hypothesis of crustal contamination is favored by the high temperatures reached by crustal rocks as a consequence of repetitive intrusions of magma. From the ‘deep’ reservoir magmas rise to form ‘shallow’ magma chambers at different depths, as already known in the literature, where they can undergo low-pressure differentiation and mixing and feed the volcanic activity. | en |
| dc.format.extent | 487 bytes | en |
| dc.format.extent | 546764 bytes | en |
| dc.format.mimetype | text/html | en |
| dc.format.mimetype | application/pdf | en |
| dc.language.iso | English | en |
| dc.publisher.name | Elsevier | en |
| dc.relation.ispartof | Journal of volcanology and geothermal research | en |
| dc.relation.ispartofseries | 133 | en |
| dc.subject | Magmatic system | en |
| dc.subject | Crustal contamination | en |
| dc.subject | Thermal modeling | en |
| dc.subject | Isotope geochemistry | en |
| dc.title | Thermal and geochemical constraints on the ‘deep’ magmatic structure of Mt. Vesuvius | en |
| dc.type | article | en |
| dc.description.status | Published | en |
| dc.type.QualityControl | Peer-reviewed | en |
| dc.description.pagenumber | 1-12 | en |
| dc.identifier.URL | www.elsevier.com/locate/jvolgeores | en |
| dc.subject.INGV | 04. Solid Earth::04.08. Volcanology::04.08.03. Magmas | en |
| dc.identifier.doi | 10.1016/S0377-0273(03)00387-1 | en |
| dc.relation.references | Andronico, D., Calderoni, G., Cioni, R., Sbrana, A., Sulpizio, R., Santacroce, R., 1995. Geological map of Somma-Vesuvius volcano. Per. Mineral. 64, 77^78. Auger, E., Gasparini, P., Virieux, J., Zollo, A., 2001. Seismic evidence of an extended magmatic sill under Mt. Vesuvius. Science 294, 1510^1512. Ayuso, R.A., De Vivo, B., Rolandi, G., Seal, I.I.R.R., Paone, A., 1998. Geochemical and isotopic (Nd^Pb^Sr^O) variations bearing on the genesis of volcanic rocks from Vesuvius, Italy. J. Volcanol. Geotherm. Res. 82, 53^78. Barberi, F., Bizouard, H., Clocchiatti, R., Me.trich, N., Santacroce, R., Sbrana, A., 1981. The Somma-Vesuvius magma chamber: A petrological and vulcanological approach. Bull. Volcanol. 44, 295^315. Belkin, H.E., De Vivo, B., 1993. Fluid inclusion studies of ejected nodules from plinian eruptions of Mt. Somma-Vesuvius. J. Volcanol. Geotherm. Res. 58, 89^100. Belkin, H.E., De Vivo, B., Roedder, E., Cortini, M., 1985. Fluid inclusion geobarometry from ejected Mt. Somma-Vesuvius nodules. Am. Mineral. 70, 288^303. Bianco, F., Castellano, M., Milano, G., Ventura, G., Vilardo, G., 1998. The Somma-Vesuvius stress field induced by regional tectonics : Evidences by seismological and mesostructural data. J. Volcanol. Geotherm. Res. 82, 199^218. Brocchini, D., Principe, C., Castradori, D., Laurenzi, M.A., Gorla, L., 2001. Quaternary evolution of the southern sector of the Campanian Plain and early Somma^Vesuvius activity: Insights from the Trecase 1 well. Mineral. Petrol. 73, 67^91. Bruno, P.P.G., Cippitelli, G., Rapolla, A., 1998. Seismic study of the Mesozoic carbonate basement around Mt. Somma^-Vesuvius, Italy. J. Volcanol. Geotherm. Res. 84, 311^322. Caprarelli, G., Togashi, S., De Vivo, B., 1993. Preliminary Sr and Nd isotopic data for recent lavas from Vesuvius volcano. J. Volcanol. Geotherm. Res. 58, 377^381. Carslaw, H.S., Jaeger, J.C., 1959. Conduction of Heat in Solids. Clarendon Press, Oxford. Cioni, R., Civetta, L., Marianelli, P., Metrich, N., Santacroce, R., Sbrana, A., 1995. Compositional layering and syn-eruptive mixing of a periodically re￠lled shallow magma chamber: The AD 79 plinian eruption of Vesuvius. J. Petrol. 36, 739^776. Cioni, R., Marianelli, P., Santacroce, R., 1998. Thermal and compositional evolution of the shallow magma chambers of Vesuvius : Evidence from pyroxene phenocrysts and melt inclusions. J. Geophys. Res. 103, 18277^18294. Cioni, R., Marianelli, P., Santacroce, R., 1999. Temperature of Vesuvius magmas. Geology 27, 443^446. Civetta, L., D’Antonio, M., Paone, E., Santacroce, R., 1987. Isotopic studies of the products of the 472 A.D. Pollena eruption (Somma^Vesuvius). Boll. G.N.V. III, 263^271. Civetta, L., Galati, R., Santacroce, R., 1991a. Magma mixing and convective compositional layering within the Vesuvius magma chamber. Bull. Volcanol. 53, 287^300. Civetta, L., Gallo, G., Orsi, G., 1991b. Sr- and Nd-isotope and trace-element constraints on the chemical evolution of the magmatic system of Ischia (Italy) in the last 55 ka. J. Volcanol. Geotherm. Res. 46, 213^230. Civetta, L., Santacroce, R., 1992. Steady state magma supply in the last 3400 years of Vesuvius activity. Acta Vulcanol. 2, 147^159. Cochran, R., 1983. Effects of ￠nite rifting times on the development of sedimentary basins. Earth Planet. Sci. Lett. 66, 289^302. Cortini, M., Hermes, O.D., 1981. Sr isotopic evidence for a multi-source origin of the potassic magmas in the Neapolitan area (S. Italy). Contrib. Mineral. Petrol. 77, 47^55. D’Antonio, M., Civetta, L., Arienzo, I., Carandente, A., Di Renzo, V., Di Vito, M.A., Giordano, F., Orsi, G., 2003. Magmatic history of Mt. Vesuvius on the basis of new geochemical and isotopic data. J. Petrol. (in press). D’Antonio, M., Civetta, L., Di Girolamo, P., 1999a. Mantle Source heterogeneity in the Campanian Region (South Italy) as inferred from geochemical and isotopic features of mafic volcanic rocks with shoshonitic affinity. Mineral. Petrol. 67, 163^192. D’Antonio, M., Civetta, L., Orsi, G., Pappalardo, L., Piochi, M., Carandente, A., de Vita, S., Di Vito, M.A., Isaia, R., 1999b. The present state of the magmatic system of the Campi Flegrei caldera based on a reconstruction of its behaviour in the past 12 ka. J. Volcanol. Geotherm. Res. 91, 247^268. de Lorenzo, S., Zollo, A., Mongelli, F., 2001a. Source parameters and three-dimensional attenuation structure from the inversion of microearthquake pulse width data: Qp imaging and inferences on the thermal state of the Campi Flegrei caldera (southern Italy). J. Geophys. Res. 106, 16265^16286. de Lorenzo, S., Gasparini, P., Mongelli, F., Zollo, A., 2001b. Thermal state of the Campi Flegrei caldera inferred from seismic attenuation tomography. J. Geodyn. 32, 467^487. De Matteis, R., Latorre, D., Zollo, A., Virieux, J., 2000. 1D P-velocity models of Mt. Vesuvius volcano from the inversion of TomoVes96 first arrival time data. Pure Appl. Geophys. 157, 1643^1661. Di Maio, R., Mauriello, P., Patella, D., Petrillo, Z., Piscitelli, S., Siniscalchi, A., 1998. Electric and electromagnetic outline of the Mount Somma^Vesuvius structural setting. J. Volcanol. Geotherm. Res. 82, 219^238. Dragoni, M., Harabaglia, P., Mongelli, F., 1997. Stress field at transcurrent plate boundary in the presence of frictional heat production at depth. Pure Appl. Geophys. 150, 181^201. Fedi, M., Florio, G., Rapolla, A., 1998. 2.5D modelling of Somma^Vesuvius structure by aeromagnetic data. J. Volcanol. Geotherm. Res. 82, 239^247. Fulignati, P., Marianelli, P., Sbrana, A., 1998. New insights on the thermometamorphic metasomatic magma chamber shell of the 1944 eruption of Vesuvius. Acta Vulcanol. 10, 47^54. Gasparini, P., Capuano, P., Virieux, J., Zollo, A., Casale, R. (Eds.), 2001. Internal Structure of Mt. Vesuvius through 3D high Resolution seismic Tomography. Eur. Comm., Direct. Gen. XII, Science, Research and Development, Environment and Climate, Proj. ENV4-980698, 130 pp. George, M.T., Bartlett, J.M., 1996. Rejuvenation of Rb^Sr mica ages during shearing on the northwestern margin of the Nanga Parbat^Haramosh massif. Tectonophysics 260, 167^185. Graham, D.W., Allard, P., Kilburn, C.R.J., Spera, F.J., Lupton, J.E., 1993. Helium isotopes in some historical lavas from Mount Vesuvius. J. Volcanol. Geotherm. Res. 58, 359^366. Hawkesworth, C.J., Vollmer, R., 1979. Crustal contamination versus enriched mantle: 143Nd/144Nd and 87Sr/86Sr evidence from the Italian volcanics. Contrib. Mineral. Petrol. 69, 151^165. Jaeger, J.C., 1964. Thermal effect of intrusions. Rev. Geophys. 2, 443^466. Joron, J.L., Me.trich, N., Rosi, M., Santacroce, R., Sbrana, A., 1987. Chemistry and petrography. In: Santacroce, R. (Ed.), Somma^Vesuvius. C.N.R., Quaderni de ‘La Ricerca Scientifica’ 114, Rome, pp. 105^174. Lachenbruch, A.H., 1970. Crustal temperature and heat production: implication of the linear Heat Flow relation. J. Geophys. Res. 75, 3219^3300. Landenberger, B., Farrell, T.R., Offer, R., Collins, W.J., Whitford, D.J., 1995. Tectonic implications of Rb^Sr biotite ages for the Hillgrove Plutonic Suite, New England Fold Belt, N.S.W. Australia. Precambrian Res. 71, 252^263. Lomax, A., Zollo, A., Capuano, P., 2001. Precise, absolute, earthquake location under Somma Vesuvius using a new 3D velocity model. Geophys. J. Int. 146, 316^331. Marianelli, P., Metrich, N., Santacroce, R., Sbrana, A., 1995. Mafic magma batches at Vesuvius: A glass inclusion approach to the modalities of feeding stratovolcanoes. Contrib. Mineral. Petrol. 120, 159^169. Marianelli, P., Metrich, N., Sbrana, A., 1999. Shallow and deep reservoirs involved in magma supply of the 1944 eruption of Vesuvius. Bull. Volcanol. 61, 48^63. Mongelli, F., Zito, G., de Lorenzo, S., 2000. Thermal effects of long intrusions. Geothermics 29, 347^365. Panza, G.F., Suhadolc, P., 1990. Properties of the lithosphere in collisional belts in the Mediterranean - a review. Tectonophysics 182, 39^46. Pappalardo, L., Civetta, L., D’Antonio, M., Deino, A., Di Vito, M.A., Orsi, G., Carandente, A., de Vita, S., Isaia, R., Piochi, M., 1999. Chemical and Sr-isotopical evolution of the Phlegraean magmatic system before the Campanian Ignimbrite (37 ka) and the Neapolitan Yellow Tu! (12 ka) eruptions. J. Volcanol. Geotherm. Res. 91, 141^166. Pappalardo, L., Piochi, M., D’Antonio, M., Civetta, L., Petrini, R., 2002. Evidence for multi-stage magmatic evolution during the past 60 kyr at Campi Flegrei (Italy) deduced from Sr, Nd and Pb isotope data. J. Petrol. 43, 1415^1434. Principe, C., Rosi, M., Santacroce, R., Sbrana, A., 1987. Explanatory note to the geological map. In: Santacroce, R. (Ed.), Somma^Vesuvius. C.N.R., Quaderni de ‘La Ricerca Scientifica’ 114, Rome, pp. 11^52. Santacroce, R., 1983. A general model for the behavior of the Somma^Vesuvius volcanic complex. J. Volcanol. Geotherm. Res. 17, 237^248. Santacroce, R. (Ed.), 1987. Somma^Vesuvius. C.N.R., Quaderni de ‘La Ricerca Scientifica’ 114, Rome, 251 pp. Santacroce, R., Bertagnini, A., Civetta, L., Landi, P., Sbrana, A., 1993. Eruptive dynamics and petrogenetic processes in a very shallow magma reservoir: The 1906 eruption of Vesuvius. J. Petrol. 34, 383^425. Santacroce, R., Cioni, R., Civetta, L., Marianelli, P., Metrich, N., 1994. How Vesuvius works. Atti Conv. Lincei 112, 185^196. Somma, R., Ayuso, R.A., De Vivo, B., Rolandi, G., 2001. Major, trace element and isotope geochemistry (Sr^Nd^Pb) of interplinian magmas from Mt. Somma^Vesuvius (Southern Italy). Mineral. Petrol. 73, 121^143. Tilton, G., Ames, L., Schertl, H.-P., Schreyer, W., 1997. Reconnaissance isotopic investigations on rocks of an undeformed granite contact within the coesite-bearing unit of the Dora Maira Massif. Lithos 41, 25^36. Thompson, A.B., 2001. Clockwise P^T paths for crustal melting and H2O recycling in granite source regions and migmatite terrains. Lithos 56, 33^45. Tonarini, S., Leeman, W.P., Civetta, L., D’Antonio, M., Ferrara, G., Necco, A., 2004. B/Nb and N11B systematics in the Phlegrean Volcanic District (PVD). J. Volcanol. Geotherm. Res. this volume, doi: 10.1016/S0377-0273(03)00394-9. Trigila, R., De Natale, G., Dol￠, D., Troise, C., 2000. Melt quenching with magma chambers after explosive or mixed eruptions: The case of Vesuvius. Geophys. Res. Abstr. 2, 1. Turi, B., Taylor, H.P., Jr., 1976. Oxygen isotope studies of potassic volcanic rocks of the roman province, central Italy. Contrib. Mineral. Petrol. 55, 1^31. Turi, B., Taylor, H.P. Jr., Ferrara, G., 1991. Comparison of 18O/16O and 87Sr/86Sr in volcanic rocks from the Pontine Islands, M. Ernici, and Campania with other areas in Italy. In: Taylor, H.P., O’Neal, J.R., Kaplan, I.R. (Eds.), Stable Isotope Geochemistry: A Tribute to Samuel Epstain. The Geochemical Society, Spec. Publ. 3, pp. 307^324. Vollmer, R., Hawkesworth, C.J., 1980. Lead isotopic composition of the potassic rocks from Roccamonfina (South Italy). Earth Planet. Sci. Lett. 47, 91^101. Wohletz, K., Civetta, L., Orsi, G., 1999. Thermal evolution of the Phlegraean magmatic system. J. Volcanol. Geotherm. Res. 91, 381^414. Wyllie, P.J., 1977. Crustal anatexis: An experimental review. Tectonophysics 43, 41^71. Yang, P., Rivers, T., 2000. Trace element partitioning between coexisting biotite and muscovite from metamorphic rocks, Western Labrador : Structural, compositional and thermal controls. Geochim. Cosmochim. Acta 64, 1451^1472. Zollo, A., Gasparini, P., Virieux, J., Biella, G., Boschi, E., Capuano, P., de Franco, R., Dell’Aversana, P., De Matteis, R., De Natale, G., Iannaccone, G., Guerra, I., Le Meur, H., Mirabile, L., 1998. An image of Mt. Vesuvius obtained by 2D seismic tomography. J. Volcanol. Geotherm. Res. 82, 161^173. Zollo, A., Gasparini, P., Virieux, J., Le Meur, H., De Natale, G., Biella, G., Boschi, E., Capuano, P., de Franco, R., Dell’Aversana, P., De Matteis, R., Guerra, I., Iannaccone, G., Mirabile, L., Vilardo, G., 1996. Seismic evidence for a low-velocity zone in the upper crust beneath Mount Vesuvius. Science 274, 592^594. Zollo, A., Marzocchi, W., Capuano, P., Lomax, A., Iannaccone, G., 2002. Space and time behaviour of seismic activity at Mt. Vesuvius volcano, Southern Italy. Bull. Seismol. Soc. Am. 92, 625^640. | en |
| dc.description.fulltext | partially_open | en |
| dc.contributor.author | Civetta, L. | en |
| dc.contributor.author | D'Antonio, M. | en |
| dc.contributor.author | de Lorenzo, S. | en |
| dc.contributor.author | Di Renzo, V. | en |
| dc.contributor.author | Gasparini, P. | en |
| dc.contributor.department | Istituto Nazionale di Geofisica e Vulcanologia, Sezione OV, Napoli, Italia | en |
| dc.contributor.department | Istituto Nazionale di Geofisica e Vulcanologia, Sezione OV, Napoli, Italia | en |
| dc.contributor.department | Dip. Geologia e Geofisica, University of Bari, Bari | en |
| dc.contributor.department | Istituto Nazionale di Geofisica e Vulcanologia, Sezione OV, Napoli, Italia | en |
| dc.contributor.department | Dip. Scienze Fisiche, Università Federico II, Napoli | 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 | Istituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione OV, Napoli, Italia | - |
| crisitem.author.dept | Università di Napoli "Federico II" | - |
| crisitem.author.dept | Dipartimento di Scienze della Terra e Geoambientali, University of Bari, Italy | - |
| crisitem.author.dept | Istituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione OV, Napoli, Italia | - |
| crisitem.author.orcid | 0000-0003-2504-1485 | - |
| crisitem.author.orcid | 0000-0002-0859-0856 | - |
| crisitem.author.parentorg | Istituto Nazionale di Geofisica e Vulcanologia | - |
| crisitem.author.parentorg | Istituto Nazionale di Geofisica e Vulcanologia | - |
| crisitem.classification.parent | 04. Solid Earth | - |
| crisitem.department.parentorg | Istituto Nazionale di Geofisica e Vulcanologia | - |
| crisitem.department.parentorg | Istituto Nazionale di Geofisica e Vulcanologia | - |
| crisitem.department.parentorg | Istituto Nazionale di Geofisica e Vulcanologia | - |
| Appears in Collections: | Article published / in press | |
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