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Pb Isotopes Data from the Campanian Volcanic Province: A Model to Generate These Distinctive Pb Isotopic Variations

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ABSTRACT
A broad set of samples from the CVP has been analyzing Pb isotopes. Campanian Volcanic Province (CVP) has been produced by various ranges of mixing between three components: 1) MORB, 2) Hercynian basement and 3) upper crust. Anyhow, the upper crust that has modified the Pb isotopic composition also shows trends towards an Achaean upper crust. This is consistent for all Mediterranean area. This is not in contrast with the past plate tectonic reconstruction. Also the surface sediments (GLOSS) may have been a mixing between the Achaean upper crust and a Hercynian component with an implication worldwide due to the rock cycle processes.
 
Cite this paper
Paone, A. (2015) Pb Isotopes Data from the Campanian Volcanic Province: A Model to Generate These Distinctive Pb Isotopic Variations. Open Journal of Geology, 5, 1-12. doi: 10.4236/ojg.2015.51001.
 
References
[1]Paone, A. (2006) The Geochemical Evolution of Somma-Vesuvius Volcano. Mineralogy and Petrology, 87, 53-80. http://dx.doi.org/10.1007/s00710-005-0103-7
 
[2]Pappalardo, L., Piochi, M., D’Antonio, M., Civetta, L. and Petrini, R. (2002) Evidence for Multistage Magmatic Evolution during the Past 60 kyr at Campi Flegrei (Italy) Deduced from Sr, Nd, and Pb Isotope Data. Journal of Petroleum, 43, 1415-1434. http://dx.doi.org/10.1093/petrology/43.8.1415
 
[3]Paone, A. (2004) Evidence of Crustal Contamination, Sediment, and Fluid Components in the Campanian Volcanic Rocks. Journal of Volcanology and Geothermal Research, 138, 1-26.
http://dx.doi.org/10.1093/petrology/43.8.1415
 
[4]Paone, A. (2013) Petrogenesis of Trachyte and Rhyolite Magmatism on Ponza Island (Italy) and Its Relationship to the Campanian Magmatism. Journal of Volcanology and Geothermal Research, 267, 15-29. http://dx.doi.org/10.1016/j.jvolgeores.2013.09.008
 
[5]Annen, C. and Sparks, R.S.J. (2002) Effects of Repetitive Emplacement of Basaltic Intrusions on Thermal Evolution and Melt Generation in the Deep Crust. Earth Planet. Science Letters, 203, 937-955.
http://dx.doi.org/10.1016/S0012-821X(02)00929-9
 
[6]Annen, C., Blundy, J.D. and Sparks, R.S.J. (2006) The Genesis of Intermediate and Silicic Magmasin Deep Crustal Hot Zones. Journal of Petrology, 47, 505-539. http://dx.doi.org/10.1093/petrology/egi084
 
[7]D’Antonio, M., Civetta, L. and Di Girolamo, P. (1999) Mantle Source Heterogeneity in the Campanian Region (South Italy) as Inferred from Geochemical and Isotopic Features of Mafic Volcanic Rocks with Shoshonitic Affinity. Mineralogy and Petrology, 67, 163-192. http://dx.doi.org/10.1007/BF01161520
 
[8]Scrocca, D., Doglioni, C. and Innocenti, F. (2003) Constraints for an Interpretation of the Italian Geodynamics: A Review. Memorie descrittive della carta geologica d’Italia Servizio geologico d’Italia, 62, 15-46.
 
[9]Doe, B.R. (1970) Lead Isotopes. Minerals, Rocks and Inorganic Materials. Monograph Series of Theoretical and Experimental Studies 3. Springer, Berlin, 143.
 
[10]Faure, G. and Mensing, T.M. (2004) Isotopes: Principles and Applications. John Wiley and Sons, Hoboken, 897.
 
[11]Dickin, A.P. (2005) Radiogenic Isotope Geology. 2nd Edition, Cambridge University Press, Cambridge, 509. http://dx.doi.org/10.1017/CBO9781139165150
 
[12]Picarelli, L., Evangelista, A., Rolandi, G., Paone, A., Nicotera, M., Olivares, L., Scotto di Santolo, A., Lampitiello, S. and Rolandi, M. (2006) Mechanical Properties and Behaviour of Pyroclastic Soils in Campania Region. Proceedings of the 2nd International Workshop on Characterisation and Engineering Properties of Natural Soils, Singapore, 29 November-1 December 2006, 2331-2384.
 
[13]De Vivo, B., Rolandi, G., Gans, P.B., Calvert, A., Bohrson, B.A., Spera, F.J. and Belkin, H.E. (2001) New Constraints on the Pyroclastic Eruptive History of the Campanian Volcanic Plain (Italy). Mineralogy and Petrology, 73, 47-65. http://dx.doi.org/10.1007/s007100170010
 
[14]De Vivo, B., Torok, K., Ayuso, R.A., Lima, A. and Lirer, L. (1995) Fluid Inclusion Evidence for Magmatic Silicate/Saline/CO2 Immiscibility and Geochemistry of Alkaline Xenoliths from Ventotene Island, Italy. Geochimica et Cosmochimica Acta, 59, 2941-2953. http://dx.doi.org/10.1016/0016-7037(95)00186-7
 
[15]Ito, E., White, W.M. and Gopel, C. (1987) The O, Sr, Nd and Pb Isotope Geochemistry of MORB. Chemical Geology, 62, 157-176. http://dx.doi.org/10.1016/0009-2541(87)90083-0
 
[16]Rollinsson, H.G. (1993) Using Geochemical Data: Evaluation, Presentation, Interpretation. Pearson Education Limited, Harlow, 380.
 
[17]Rottura, A., Del Moro, A., Pinarelli, L., Petrini, R., Peccerillo, A., Caggianelli, G.M. and Piccarretta, G. (1991) Relationships between Intermediate and Acidic Rocks in Orogenic Granitoid Suites: Petrological, Geochemical and Isotopic (Sr, Nd, Pb) Data from Capo Vaticano (Southern Calabria, Italy). Chemical Geology, 92, 153-176. http://dx.doi.org/10.1016/0009-2541(91)90054-U
 
[18]Ayuso, R.A., Messina, A., De Vivo, B., Russo, S., Woodruff, L.G., Sutter, J.F. and Belkin, H.E. (1994) Geochemistry and Argon Thermochronology of the Variscan Sila Batholith, Southern Italy: Source Rocks and Magma Evolution. Contributions to Mineralogy and Petrology, 117, 87-109.
http://dx.doi.org/10.1007/BF00307732
 
[19]Plank, T. and Langmuir, C.H. (1998) The Composition of Subducting Sediment and Its Consequences for the Crust and Mantle. Chemical Geology, 145, 325-394.
http://dx.doi.org/10.1016/S0009-2541(97)00150-2
 
[20]Paone, A. (2013) A Review of Carbonatite Occurrences in Italy and Evaluation of Origins. Open Journal of Geology, 3, 66-82. http://dx.doi.org/10.4236/ojg.2013.32011                                        eww150122lx

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