Petrogenesis of the high-alumina basalt-andesite suite from Sant'Antioco island, SW Sardinia, Italy. (Articolo in rivista)

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  • Petrogenesis of the high-alumina basalt-andesite suite from Sant'Antioco island, SW Sardinia, Italy. (Articolo in rivista) (literal)
Anno
  • 2010-01-01T00:00:00+01:00 (literal)
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  • 10.2451/2010PM0002 (literal)
Alternative label
  • Conte A.M.; Palladino D.M.; Perinelli C.; Argenti E. (2010)
    Petrogenesis of the high-alumina basalt-andesite suite from Sant'Antioco island, SW Sardinia, Italy.
    in Periodico di mineralogia (Testo stamp.)
    (literal)
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  • Conte A.M.; Palladino D.M.; Perinelli C.; Argenti E. (literal)
Pagina inizio
  • 27 (literal)
Pagina fine
  • 55 (literal)
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  • 79 (literal)
Rivista
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  • In: Periodico di Mineralogia, vol. 79 (1) pp. 27 - 55. Dipartimento di Scienze della Terra, Università degli Studi La Sapienza, Roma, 2010. (literal)
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  • 29 (literal)
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  • 1 (literal)
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  • Conte: C.N.R.- I.G.G.- U.O.S.di Roma, Dipartimento di Scienze della Terra, Sapienza Università di Roma, P.le Aldo Moro 5, Roma, Italy Palladino: Dipartimento di Scienze della Terra, Sapienza Università di Roma, P.le Aldo Moro 5, 00185 Roma, Italy Perinelli: Dipartimento di Scienze della Terra, Università di Pisa, Via Santa Maria 53, 56126 Pisa, Italy Argenti: Parco Naturale Regionale Bracciano Martignano, Via A. Saffi, 4/A, Bracciano, 00062 Roma, Italy (literal)
Titolo
  • Petrogenesis of the high-alumina basalt-andesite suite from Sant'Antioco island, SW Sardinia, Italy. (literal)
Abstract
  • Present-day Sant'Antioco Island (SW-Sardinia, Italy) hosted one of the southernmost, and youngest, subduction-related, Cenozoic magmatic events of western Sardinia. A high-alumina basalt-andesite rock association, the focus of this paper, crops out in the southern portion of the island and represents the mafic end-member of volcanism developed during Miocene. Basaltic andesites and andesites are the dominant rock-types, while basalts and dacites are occasional. Minero-petrographic and geochemical characteristics reveal: i) a clear calc-alkaline signature for these rocks, in spite of high FeO*/MgO ratios that mimic a tholeiitic affinity; ii) a magma evolution mainly controlled by fractional crystallization and iii) some degree of crustal assimilation. Phase relationships and compositions, mass balance calculations and T, P, XH2O estimates consistently indicate that fractional crystallization occurred at low pressure (P=100-400 MPa), under different PH2O conditions, which explain the observed wide shifts in major oxides (e.g., Al2O3 and MgO), for comparable SiO2 contents, and the ambiguous tholeiitic character as well. Phase relationships in the least evolved lithotypes point out that higher H2O concentrations (estimated at up to 6 wt%) in the melts reduced the crystallization of plagioclase and favoured that of olivine, whereas lower H2O contents (up to 3 wt%) promoted plagioclase fractionation and earlier crystallization of orthopyroxene at the expense of olivine. this XH2O imprint was recorded up to the most evolved compositions. Finally, the study rock suite can be derived from a parental (near-primary) magma matching in composition high-MgO basalts from the Montresta calc-alkaline district in NW sardinia, in the light of the close compositional similarity between the high-Al2O3 basaltic andesites in the two districts. Thus, starting from a common parental composition, here we reconstruct liquid lines of descent, where the relative proportions of fractionating pla (literal)
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