FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2006119107> ?p ?o ?g. }

• W2006119107 endingPage "167" @default.
• W2006119107 startingPage "148" @default.
• W2006119107 abstract "The Nonsberg–Ultental Region of northern Italy contains a Palaeozoic mélange that was partially subducted during the Variscan orogeny. This mélange is constituted mainly by metapelites characterized by shale-type REE-patterns, displaying partial melting which began under high-pressure conditions. The resulting migmatites enclose minor slivers of mantle-wedge peridotites that have been incorporated into the mélange during subduction. Peridotites display important large ion lithophile elements (LILE) enrichment consequent to amphibole recrystallization contemporaneously with metapelite migmatization at P ≈ 2.7 GPa and T ≈ 850 °C in the garnet–peridotite field. Crustal and mantle (ultramafic) rocks of the mélange display the same Sm–Nd ages of about 330 ± 6 Ma, which dates both the metamorphic peak and the migmatization event. The zircon U–Pb age of the metasomatic amphibolitic contact between garnet peridotite and migmatite is identical (333.3 ± 2.4 Ma) within analytical errors. Therefore, metasomatism, migmatization and peak metamorphism are constrained to the same event. The presence of Cl-rich apatite and ferrokinoshitalite in the contact amphibolite, together with the trace-element patterns of peridotites, suggest that metasomatism was driven by Cl- and LILE-rich fluids derived from ocean water transported into the subduction zone by sediments and crustal rocks. These fluids interacted with the crust, prompting partial melting under water oversaturated conditions and partitioning LILE from the crust itself. Peridotites, which were well below their wet solidus temperature, could not melt but they recrystallized in the crustal mélange under garnet-facies conditions. Crustal fluids caused extensive hydration and LILE-enrichment in peridotites and severe Sm–Nd isotope disequilibrium between minerals, especially in the recrystallized peridotites. The proposed scenario suggests massive entrapment of crustal aqueous fluids at high-pressure conditions within subduction zones." @default.
• W2006119107 created "2016-06-24" @default.
• W2006119107 creator A5003403825 @default.
• W2006119107 creator A5005515587 @default.
• W2006119107 creator A5027893999 @default.
• W2006119107 creator A5047335601 @default.
• W2006119107 creator A5077828630 @default.
• W2006119107 date "2007-03-01" @default.
• W2006119107 modified "2023-10-17" @default.
• W2006119107 title "Fluid-controlled crustal metasomatism within a high-pressure subducted mélange (Mt. Hochwart, Eastern Italian Alps)" @default.
• W2006119107 cites W1633155736 @default.
• W2006119107 cites W1965434351 @default.
• W2006119107 cites W1966256034 @default.
• W2006119107 cites W1966707406 @default.
• W2006119107 cites W1969793102 @default.
• W2006119107 cites W1972887299 @default.
• W2006119107 cites W2007105153 @default.
• W2006119107 cites W2007976131 @default.
• W2006119107 cites W2008184556 @default.
• W2006119107 cites W2020523848 @default.
• W2006119107 cites W2023691463 @default.
• W2006119107 cites W2055966923 @default.
• W2006119107 cites W2058564431 @default.
• W2006119107 cites W2068751740 @default.
• W2006119107 cites W2080986287 @default.
• W2006119107 cites W2115443754 @default.
• W2006119107 cites W2163699960 @default.
• W2006119107 cites W2170091491 @default.
• W2006119107 cites W2587529116 @default.
• W2006119107 cites W406392054 @default.
• W2006119107 cites W4245500528 @default.
• W2006119107 doi "https://doi.org/10.1016/j.lithos.2006.06.009" @default.
• W2006119107 hasPublicationYear "2007" @default.
• W2006119107 type Work @default.
• W2006119107 sameAs 2006119107 @default.
• W2006119107 citedByCount "32" @default.
• W2006119107 countsByYear W20061191072012 @default.
• W2006119107 countsByYear W20061191072015 @default.
• W2006119107 countsByYear W20061191072017 @default.
• W2006119107 countsByYear W20061191072018 @default.
• W2006119107 countsByYear W20061191072020 @default.
• W2006119107 countsByYear W20061191072021 @default.
• W2006119107 countsByYear W20061191072022 @default.
• W2006119107 countsByYear W20061191072023 @default.
• W2006119107 crossrefType "journal-article" @default.
• W2006119107 hasAuthorship W2006119107A5003403825 @default.
• W2006119107 hasAuthorship W2006119107A5005515587 @default.
• W2006119107 hasAuthorship W2006119107A5027893999 @default.
• W2006119107 hasAuthorship W2006119107A5047335601 @default.
• W2006119107 hasAuthorship W2006119107A5077828630 @default.
• W2006119107 hasConcept C109007969 @default.
• W2006119107 hasConcept C112764850 @default.
• W2006119107 hasConcept C114793014 @default.
• W2006119107 hasConcept C119073576 @default.
• W2006119107 hasConcept C127313418 @default.
• W2006119107 hasConcept C146588470 @default.
• W2006119107 hasConcept C151730666 @default.
• W2006119107 hasConcept C167919410 @default.
• W2006119107 hasConcept C171701179 @default.
• W2006119107 hasConcept C17409809 @default.
• W2006119107 hasConcept C18142444 @default.
• W2006119107 hasConcept C26687426 @default.
• W2006119107 hasConcept C2777241186 @default.
• W2006119107 hasConcept C2780040746 @default.
• W2006119107 hasConcept C58097730 @default.
• W2006119107 hasConcept C5900021 @default.
• W2006119107 hasConcept C67236022 @default.
• W2006119107 hasConcept C73462661 @default.
• W2006119107 hasConcept C77928131 @default.
• W2006119107 hasConcept C79572550 @default.
• W2006119107 hasConcept C84372278 @default.
• W2006119107 hasConceptScore W2006119107C109007969 @default.
• W2006119107 hasConceptScore W2006119107C112764850 @default.
• W2006119107 hasConceptScore W2006119107C114793014 @default.
• W2006119107 hasConceptScore W2006119107C119073576 @default.
• W2006119107 hasConceptScore W2006119107C127313418 @default.
• W2006119107 hasConceptScore W2006119107C146588470 @default.
• W2006119107 hasConceptScore W2006119107C151730666 @default.
• W2006119107 hasConceptScore W2006119107C167919410 @default.
• W2006119107 hasConceptScore W2006119107C171701179 @default.
• W2006119107 hasConceptScore W2006119107C17409809 @default.
• W2006119107 hasConceptScore W2006119107C18142444 @default.
• W2006119107 hasConceptScore W2006119107C26687426 @default.
• W2006119107 hasConceptScore W2006119107C2777241186 @default.
• W2006119107 hasConceptScore W2006119107C2780040746 @default.
• W2006119107 hasConceptScore W2006119107C58097730 @default.
• W2006119107 hasConceptScore W2006119107C5900021 @default.
• W2006119107 hasConceptScore W2006119107C67236022 @default.
• W2006119107 hasConceptScore W2006119107C73462661 @default.
• W2006119107 hasConceptScore W2006119107C77928131 @default.
• W2006119107 hasConceptScore W2006119107C79572550 @default.
• W2006119107 hasConceptScore W2006119107C84372278 @default.
• W2006119107 hasIssue "1-4" @default.
• W2006119107 hasLocation W20061191071 @default.
• W2006119107 hasLocation W20061191072 @default.
• W2006119107 hasLocation W20061191073 @default.
• W2006119107 hasOpenAccess W2006119107 @default.
• W2006119107 hasPrimaryLocation W20061191071 @default.

• next