Item talk:Q250790

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{

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   "name": "Formation of cordierite-bearing lavas during anatexis in the lower crust beneath Lipari Island (Aeolian arc, Italy)",
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   "abstract": "Cordierite-bearing lavas (CBL;~105\u00a0ka) erupted from the Mt. S. Angelo volcano at Lipari (Aeolian arc, Italy) are high-K andesites, displaying a range in the geochemical and isotopic compositions that reflect heterogeneity in the source and/or processes. CBL consist of megacrysts of Ca-plagioclase and clinopyroxene, euhedral crystals of cordierite and garnet, microphenocrysts of orthopyroxene and plagioclase, set in a heterogeneous rhyodacitic-rhyolitic groundmass containing abundant metamorphic and gabbroic xenoliths. New petrographic, chemical and isotopic data indicate formation of CBL by mixing of basaltic-andesitic magmas and high-K peraluminous rhyolitic magmas of anatectic origin and characterize partial melting processes in the lower continental crust of Lipari. Crustal anatectic melts generated through two main dehydration-melting peritectic reactions of metasedimentary rocks: (1) Biotite\u00a0+\u00a0Aluminosilicate\u00a0+\u00a0Quartz\u00a0+\u00a0Albite\u00a0=\u00a0Garnet\u00a0+\u00a0Cordierite\u00a0+\u00a0K-feldspar\u00a0+\u00a0Melt; (2) Biotite\u00a0+\u00a0Garnet\u00a0+\u00a0Quartz\u00a0=\u00a0Orthopyroxene\u00a0+\u00a0Cordierite\u00a0+\u00a0K-feldspar\u00a0+\u00a0Melt. Their position into the petrogenetic grid suggests that heating and consequent melting of metasedimentary rocks occurred at temperatures of 725\u00a0<\u00a0T\u00a0<\u00a0900\u00b0C and pressures of 0.4\u20130.45\u00a0GPa. Anatexis in the lower crust of Lipari was induced by protracted emplacement of basic magmas in the lower crust (~130\u00a0Ky). Crustal melting of the lower crust at 105\u00a0ka affected the volcano evolution, impeding frequent mafic-magma eruptions, and promoting magma stagnation and fractional crystallization processes.",
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