Item talk:Q250790
From geokb
{
"USGS Publications Warehouse": { "@context": "https://schema.org", "@type": "Article", "additionalType": "Journal Article", "name": "Formation of cordierite-bearing lavas during anatexis in the lower crust beneath Lipari Island (Aeolian arc, Italy)", "identifier": [ { "@type": "PropertyValue", "propertyID": "USGS Publications Warehouse IndexID", "value": "70034566", "url": "https://pubs.usgs.gov/publication/70034566" }, { "@type": "PropertyValue", "propertyID": "USGS Publications Warehouse Internal ID", "value": 70034566 }, { "@type": "PropertyValue", "propertyID": "DOI", "value": "10.1007/s00410-011-0637-0", "url": "https://doi.org/10.1007/s00410-011-0637-0" }, { "@type": "PropertyValue", "propertyID": "ISSN", "value": "00107999" } ], "journal": { "@type": "Periodical", "name": "Contributions to Mineralogy and Petrology", "volumeNumber": "162", "issueNumber": "5" }, "inLanguage": "en", "isPartOf": [ { "@type": "CreativeWorkSeries", "name": "Contributions to Mineralogy and Petrology" } ], "datePublished": "2011", "dateModified": "2021-04-16", "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.", "description": "20 p.", "publisher": { "@type": "Organization", "name": "Springer Link" }, "author": [ { "@type": "Person", "name": "Webster, J.D.", "givenName": "J.D.", "familyName": "Webster" }, { "@type": "Person", "name": "Lucchi, F.", "givenName": "F.", "familyName": "Lucchi" }, { "@type": "Person", "name": "Ayuso, R. A.", "givenName": "R. 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