Matches in SemOpenAlex for { <https://semopenalex.org/work/W1567199384> ?p ?o ?g. }
Showing items 1 to 81 of
81
with 100 items per page.
- W1567199384 endingPage "118" @default.
- W1567199384 startingPage "105" @default.
- W1567199384 abstract "The Mount Avic serpentinites derive from mantle peridotites that have been involved in several geodynamic episodes, from their formation in the Jurassic Tethys, to the subduction event and suture in the Alpine chain. The main steps of their tectono-metamorphic evolution are inferred by investigating the texture and mineralogy of selected samples. Some serpentinite samples show relict textures and mineralogy related to the emplacement in the oceanic realm and to the early Alpine evolution. Olivine and clinopyroxene porphyroblasts preserve relict mantle textures. Magnetite crystals include relict chromite at their core. Abundant pseudomorphs of antigorite on former porphyroblasts are present. Mineral composition of the pseudomorphic serpentine partly inherits the composition of former minerals (e.g., relatively Ti-rich antigorite replacing pyroxene). These observations support the hypothesis that the Mount Avic serpentinites derive from original mantle porphyroclastic peridotites. An early formation of Ti-clinohumite during oceanic serpentinization of mantle peridotites at relatively high temperature conditions, followed by HP subduction-related Alpine recrystallization, is proposed. The late orogenic history is characterised by transposition accompanied by greenschist facies minerals crystallization. In these samples, antigorite represents the main mineral phase, marking a pervasive, often mylonitic, foliation. The last generation of serpentine, that occurs as yellow fibres filling late extension veins, was formed during a Neo-Alpine brittle-ductile deformation stage." @default.
- W1567199384 created "2016-06-24" @default.
- W1567199384 creator A5003456866 @default.
- W1567199384 creator A5044740643 @default.
- W1567199384 creator A5067471600 @default.
- W1567199384 date "2008-01-07" @default.
- W1567199384 modified "2023-09-26" @default.
- W1567199384 title "OCEANIC RELICT TEXTURES IN THE MOUNT AVIC SERPENTINITES, WESTERN ALPS" @default.
- W1567199384 doi "https://doi.org/10.4454/ofioliti.v33i2.367" @default.
- W1567199384 hasPublicationYear "2008" @default.
- W1567199384 type Work @default.
- W1567199384 sameAs 1567199384 @default.
- W1567199384 citedByCount "4" @default.
- W1567199384 countsByYear W15671993842012 @default.
- W1567199384 countsByYear W15671993842015 @default.
- W1567199384 countsByYear W15671993842020 @default.
- W1567199384 crossrefType "journal-article" @default.
- W1567199384 hasAuthorship W1567199384A5003456866 @default.
- W1567199384 hasAuthorship W1567199384A5044740643 @default.
- W1567199384 hasAuthorship W1567199384A5067471600 @default.
- W1567199384 hasConcept C10912530 @default.
- W1567199384 hasConcept C127313418 @default.
- W1567199384 hasConcept C151730666 @default.
- W1567199384 hasConcept C17409809 @default.
- W1567199384 hasConcept C197737763 @default.
- W1567199384 hasConcept C23295444 @default.
- W1567199384 hasConcept C26687426 @default.
- W1567199384 hasConcept C2778998827 @default.
- W1567199384 hasConcept C2779870107 @default.
- W1567199384 hasConcept C2780364934 @default.
- W1567199384 hasConcept C2781150389 @default.
- W1567199384 hasConcept C37045145 @default.
- W1567199384 hasConcept C58097730 @default.
- W1567199384 hasConcept C67236022 @default.
- W1567199384 hasConcept C77928131 @default.
- W1567199384 hasConceptScore W1567199384C10912530 @default.
- W1567199384 hasConceptScore W1567199384C127313418 @default.
- W1567199384 hasConceptScore W1567199384C151730666 @default.
- W1567199384 hasConceptScore W1567199384C17409809 @default.
- W1567199384 hasConceptScore W1567199384C197737763 @default.
- W1567199384 hasConceptScore W1567199384C23295444 @default.
- W1567199384 hasConceptScore W1567199384C26687426 @default.
- W1567199384 hasConceptScore W1567199384C2778998827 @default.
- W1567199384 hasConceptScore W1567199384C2779870107 @default.
- W1567199384 hasConceptScore W1567199384C2780364934 @default.
- W1567199384 hasConceptScore W1567199384C2781150389 @default.
- W1567199384 hasConceptScore W1567199384C37045145 @default.
- W1567199384 hasConceptScore W1567199384C58097730 @default.
- W1567199384 hasConceptScore W1567199384C67236022 @default.
- W1567199384 hasConceptScore W1567199384C77928131 @default.
- W1567199384 hasIssue "2" @default.
- W1567199384 hasLocation W15671993841 @default.
- W1567199384 hasOpenAccess W1567199384 @default.
- W1567199384 hasPrimaryLocation W15671993841 @default.
- W1567199384 hasRelatedWork W1481720020 @default.
- W1567199384 hasRelatedWork W1576234239 @default.
- W1567199384 hasRelatedWork W1576268486 @default.
- W1567199384 hasRelatedWork W1721380001 @default.
- W1567199384 hasRelatedWork W1999147496 @default.
- W1567199384 hasRelatedWork W2005846056 @default.
- W1567199384 hasRelatedWork W2025109266 @default.
- W1567199384 hasRelatedWork W2029195908 @default.
- W1567199384 hasRelatedWork W2029742232 @default.
- W1567199384 hasRelatedWork W2031981361 @default.
- W1567199384 hasRelatedWork W2042229840 @default.
- W1567199384 hasRelatedWork W2055799604 @default.
- W1567199384 hasRelatedWork W2061249032 @default.
- W1567199384 hasRelatedWork W2082238091 @default.
- W1567199384 hasRelatedWork W2100411277 @default.
- W1567199384 hasRelatedWork W2145235529 @default.
- W1567199384 hasRelatedWork W2163081387 @default.
- W1567199384 hasRelatedWork W2291977426 @default.
- W1567199384 hasRelatedWork W2327725617 @default.
- W1567199384 hasRelatedWork W2606892490 @default.
- W1567199384 hasVolume "33" @default.
- W1567199384 isParatext "false" @default.
- W1567199384 isRetracted "false" @default.
- W1567199384 magId "1567199384" @default.
- W1567199384 workType "article" @default.