Origin and evolution of Cenozoic magmatism of Sardinia (Italy). A combined isotopic (Sr-Nd-Pb-O-Hf-Os) and petrological view

Autor: Michele Lustrino(a, Lorenzo Fedele(c), Leone Melluso (c), Vincenzo Morra (c), Fiorenzo Ronga (c), Jörg Geldmacher (d), Svend Duggen (d, e, Samuele Agostini (f), Ciro Cucciniello (c), Luigi Franciosi (c), Thomas Meisel (g)

Publikováno v: Lithos (Oslo. Print) 180-181 (2013): 138–158. doi:10.1016/j.lithos.2013.08.022
info:cnr-pdr/source/autori:Michele Lustrino(a, b), Lorenzo Fedele(c), Leone Melluso (c), Vincenzo Morra (c), Fiorenzo Ronga (c), Jörg Geldmacher (d), Svend Duggen (d,e,), Samuele Agostini (f), Ciro Cucciniello (c), Luigi Franciosi (c),Thomas Meisel (g)/titolo:Origin and evolution of Cenozoic magmatism of Sardinia (Italy). A combined isotopic (Sr-Nd-Pb-O-Hf-Os) and petrological view/doi:10.1016%2Fj.lithos.2013.08.022/rivista:Lithos (Oslo. Print)/anno:2013/pagina_da:138/pagina_a:158/intervallo_pagine:138–158/volume:180-181

The Cenozoic igneous activity of Sardinia is essentially concentrated in the 38-0.1 Myr time range. On the basis of volcanological, petrographic, mineralogical, geochemical and isotopic considerations, two main rock types can be defined. The first gr

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