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• W2076272192 abstract "Abstract Trachyte and peralkaline rhyolite (pantellerite and comendite) frequently comprise the felsic end-member in bimodal suites in continental rift and oceanic island settings. In these settings, the relationship between the mafic (mildly alkaline, or transitional, basalt) and felsic lavas is ambiguous; major- and trace-element models and isotopic data are often consistent with an origin for felsic lavas from either fractional crystallization of transitional basalt or partial melting of alkali gabbro followed by fractional crystallization. In this paper, we present representative mineral analyses and whole-rock analyses from forty samples of a basalt–trachyte–pantellerite suite collected at Pantelleria, Italy, in the Strait of Sicily Rift Zone, and compare the results of major- and trace-element modelling with the results of thermodynamic (MELTS) modelling. From these results we conclude that metaluminous trachyte formed as a result of 70 to 75% low-pressure (0.1 GPa) fractional crystallization of an assemblage of plagioclase, clinopyroxene, olivine, magnetite, and apatite from a hydrous (1.0–1.5 wt.% H2O) transitional basalt magma at relative oxygen fugacities approximately one log unit below the fayalite–magnetite–quartz buffer (FMQ−1). The “Daly gap”–a lack of intermediate (~ 49–62 wt.% SiO2) volcanic rocks–at Pantelleria is concluded to be primarily the result of rapid differentiation through that interval. Relatively rapid crystallization at low pressure may have effected the partial degassing of water-saturated (~ 4 wt.% H2O) metaluminous trachyte magma. Some metaluminous trachyte lavas have positive Eu anomalies, high K/Rb ratios, high concentrations of Ba, and low concentrations of incompatible trace elements; these are interpreted to be the result of up to 40% accumulation of alkali feldspar. Comenditic trachyte, pantelleritic trachyte, and pantellerite formed after an additional 20 to 80% fractional crystallization of an assemblage dominated by alkali feldspar from metaluminous trachyte magma. The most evolved pantellerite lavas and tuffs are the result of a total of ~ 95% fractional crystallization of transitional basalt, with phenocrysts that equilibrated at low temperatures (  4 wt.%) water contents." @default.
• W2076272192 created "2016-06-24" @default.
• W2076272192 creator A5074651230 @default.
• W2076272192 creator A5075350928 @default.
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• W2076272192 date "2009-01-01" @default.
• W2076272192 modified "2023-10-02" @default.
• W2076272192 title "The origin of trachyte and pantellerite from Pantelleria, Italy: Insights from major element, trace element, and thermodynamic modelling" @default.
• W2076272192 cites W1573196231 @default.
• W2076272192 cites W1657275263 @default.
• W2076272192 cites W1964189217 @default.
• W2076272192 cites W1965023649 @default.
• W2076272192 cites W1967375970 @default.
• W2076272192 cites W1970727466 @default.
• W2076272192 cites W1972718879 @default.
• W2076272192 cites W1974202457 @default.
• W2076272192 cites W1974487421 @default.
• W2076272192 cites W1980771119 @default.
• W2076272192 cites W1981985585 @default.
• W2076272192 cites W1984845126 @default.
• W2076272192 cites W1989829455 @default.
• W2076272192 cites W1991410913 @default.
• W2076272192 cites W1992648629 @default.
• W2076272192 cites W1995079566 @default.
• W2076272192 cites W1995671876 @default.
• W2076272192 cites W2003247029 @default.
• W2076272192 cites W2003791442 @default.
• W2076272192 cites W2006749695 @default.
• W2076272192 cites W2007421496 @default.
• W2076272192 cites W2009890298 @default.
• W2076272192 cites W2020191076 @default.
• W2076272192 cites W2021030359 @default.
• W2076272192 cites W2021247189 @default.
• W2076272192 cites W2021379806 @default.
• W2076272192 cites W2022189467 @default.
• W2076272192 cites W2023541746 @default.
• W2076272192 cites W2024634019 @default.
• W2076272192 cites W2024771628 @default.
• W2076272192 cites W2026413566 @default.
• W2076272192 cites W2028633082 @default.
• W2076272192 cites W2028635878 @default.
• W2076272192 cites W2037910514 @default.
• W2076272192 cites W2039296950 @default.
• W2076272192 cites W2039449975 @default.
• W2076272192 cites W2039704788 @default.
• W2076272192 cites W2039790603 @default.
• W2076272192 cites W2042692134 @default.
• W2076272192 cites W2046005805 @default.
• W2076272192 cites W2047984198 @default.
• W2076272192 cites W2048116571 @default.
• W2076272192 cites W2049153634 @default.
• W2076272192 cites W2050963577 @default.
• W2076272192 cites W2053970916 @default.
• W2076272192 cites W2054161635 @default.
• W2076272192 cites W2054364005 @default.
• W2076272192 cites W2062218969 @default.
• W2076272192 cites W2062274272 @default.
• W2076272192 cites W2074686196 @default.
• W2076272192 cites W2076535157 @default.
• W2076272192 cites W2077224942 @default.
• W2076272192 cites W2077418438 @default.
• W2076272192 cites W2077577717 @default.
• W2076272192 cites W2080379674 @default.
• W2076272192 cites W2081418268 @default.
• W2076272192 cites W2087295880 @default.
• W2076272192 cites W2088279173 @default.
• W2076272192 cites W2088729389 @default.
• W2076272192 cites W2092780280 @default.
• W2076272192 cites W2092836793 @default.
• W2076272192 cites W2093740880 @default.
• W2076272192 cites W2094977742 @default.
• W2076272192 cites W2095374616 @default.
• W2076272192 cites W2098018742 @default.
• W2076272192 cites W2099226696 @default.
• W2076272192 cites W2110947645 @default.
• W2076272192 cites W2117726746 @default.
• W2076272192 cites W2119905303 @default.
• W2076272192 cites W2125817863 @default.
• W2076272192 cites W2126506609 @default.
• W2076272192 cites W2129332344 @default.
• W2076272192 cites W2152821989 @default.
• W2076272192 cites W2153024854 @default.
• W2076272192 cites W2155146104 @default.
• W2076272192 cites W2159763111 @default.
• W2076272192 cites W2165073556 @default.
• W2076272192 cites W2285274212 @default.
• W2076272192 cites W2296966053 @default.
• W2076272192 cites W2324102175 @default.
• W2076272192 cites W2329112687 @default.
• W2076272192 cites W2406382646 @default.
• W2076272192 cites W4232233217 @default.
• W2076272192 cites W4234603596 @default.
• W2076272192 cites W4246695044 @default.
• W2076272192 doi "https://doi.org/10.1016/j.jvolgeores.2008.10.007" @default.
• W2076272192 hasPublicationYear "2009" @default.
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