FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2157112902> ?p ?o ?g. }

• W2157112902 endingPage "708" @default.
• W2157112902 startingPage "691" @default.
• W2157112902 abstract "The Lycian and Antalya ophiolite complexes in SW Turkey represent fragments of oceanic lithosphere emplaced following the closure of the Neotethys Ocean during the Late Cretaceous. The peridotites from both of these ophiolites have compositions ranging from relatively undepleted lherzolites to highly depleted harzburgites and display a diverse suite of geochemical signatures indicative of both anhydrous, mid-ocean ridge (MOR)-type and hydrous, supra-subduction zone (SSZ)-type melting regimes. Whole-rock major and trace element systematics and mineral chemistry indicate that the MOR- and SSZ-type peridotites represent the residues from 5–9% and 13–25% of mantle melting, respectively, and display evidence for a multi-stage evolution of an oceanic lithosphere. Olivine–orthopyroxene–spinel equilibria indicate that the clinopyroxene-bearing, MOR-type peridotites are moderately reduced with their oxygen fugacity (fO2) ranging from − 2.22 to − 1.44 log units relative to the FMQ (fayalite–magnetite–quartz) buffer and are similar to abyssal peridotites, while more refractory, SSZ-type harzburgites and dunites (< 4% modal clinopyroxene) are more oxidized with their higher oxygen fugacity (FMQ − 0.72 to + 1.02). The latter can readily be explained by interaction with oxidizing melts/fluids originating from a subducted slab in a SSZ environment. Precise determination of trace element compositions of residual clinopyroxenes by LA-ICPMS indicates that the SSZ peridotites are strongly depleted in Ti and HREE and enriched in Zr and LMREE, compared to the most depleted MOR-type peridotites. The results of quantitative model calculations show that moderate degrees of anhydrous mantle melting accounts for the composition of MOR peridotites, while SSZ peridotites are likely to have originated from hydrous, orthopyroxene-dominated remelting of previously depleted mantle. For the case of hydrous melting, it is inferred that flux of a slab-derived fluid component sustained further melting of MORB-depleted peridotite, resulting in higher degrees of depletions in the SSZ mantle than the anhydrous melting in the MOR setting. Interaction of SSZ-type melts with depleted peridotites enriched the source mantle in more incompatible trace elements, resulting in elevated Zr/Ti and LMREE/HREE ratios in peridotites. The occurrence of both MOR and SSZ styles of melting regimes indicates that these ophiolites contain mantle residues from discrete stages of oceanic lithosphere generation." @default.
• W2157112902 created "2016-06-24" @default.
• W2157112902 creator A5013236556 @default.
• W2157112902 creator A5036397423 @default.
• W2157112902 creator A5082250660 @default.
• W2157112902 creator A5091211694 @default.
• W2157112902 date "2009-12-01" @default.
• W2157112902 modified "2023-10-09" @default.
• W2157112902 title "Mid-ocean ridge and supra-subduction geochemical signatures in spinel–peridotites from the Neotethyan ophiolites in SW Turkey: Implications for upper mantle melting processes" @default.
• W2157112902 cites W1493472940 @default.
• W2157112902 cites W1535363067 @default.
• W2157112902 cites W1623919485 @default.
• W2157112902 cites W1965596457 @default.
• W2157112902 cites W1966685022 @default.
• W2157112902 cites W1967784536 @default.
• W2157112902 cites W1974505893 @default.
• W2157112902 cites W1976563860 @default.
• W2157112902 cites W1977457396 @default.
• W2157112902 cites W1978340247 @default.
• W2157112902 cites W1986708376 @default.
• W2157112902 cites W2014783682 @default.
• W2157112902 cites W2016701904 @default.
• W2157112902 cites W2028202848 @default.
• W2157112902 cites W2031295342 @default.
• W2157112902 cites W2035283420 @default.
• W2157112902 cites W2035743760 @default.
• W2157112902 cites W2036158615 @default.
• W2157112902 cites W2039064764 @default.
• W2157112902 cites W2041895575 @default.
• W2157112902 cites W2042149675 @default.
• W2157112902 cites W2057814172 @default.
• W2157112902 cites W2060655431 @default.
• W2157112902 cites W2062252830 @default.
• W2157112902 cites W2065591464 @default.
• W2157112902 cites W2071123829 @default.
• W2157112902 cites W2071583796 @default.
• W2157112902 cites W2073773279 @default.
• W2157112902 cites W2075557265 @default.
• W2157112902 cites W2087565358 @default.
• W2157112902 cites W2096168179 @default.
• W2157112902 cites W2096297752 @default.
• W2157112902 cites W2101749174 @default.
• W2157112902 cites W2104830403 @default.
• W2157112902 cites W2105663944 @default.
• W2157112902 cites W2109960134 @default.
• W2157112902 cites W2110517541 @default.
• W2157112902 cites W2112160511 @default.
• W2157112902 cites W2113369720 @default.
• W2157112902 cites W2114435682 @default.
• W2157112902 cites W2115550380 @default.
• W2157112902 cites W2118845286 @default.
• W2157112902 cites W2135015385 @default.
• W2157112902 cites W2135651322 @default.
• W2157112902 cites W2136892820 @default.
• W2157112902 cites W2138999593 @default.
• W2157112902 cites W2146904755 @default.
• W2157112902 cites W2149642705 @default.
• W2157112902 cites W2168672163 @default.
• W2157112902 cites W2316110691 @default.
• W2157112902 doi "https://doi.org/10.1016/j.lithos.2009.03.010" @default.
• W2157112902 hasPublicationYear "2009" @default.
• W2157112902 type Work @default.
• W2157112902 sameAs 2157112902 @default.
• W2157112902 citedByCount "99" @default.
• W2157112902 countsByYear W21571129022012 @default.
• W2157112902 countsByYear W21571129022013 @default.
• W2157112902 countsByYear W21571129022014 @default.
• W2157112902 countsByYear W21571129022015 @default.
• W2157112902 countsByYear W21571129022016 @default.
• W2157112902 countsByYear W21571129022017 @default.
• W2157112902 countsByYear W21571129022018 @default.
• W2157112902 countsByYear W21571129022019 @default.
• W2157112902 countsByYear W21571129022020 @default.
• W2157112902 countsByYear W21571129022021 @default.
• W2157112902 countsByYear W21571129022022 @default.
• W2157112902 countsByYear W21571129022023 @default.
• W2157112902 crossrefType "journal-article" @default.
• W2157112902 hasAuthorship W2157112902A5013236556 @default.
• W2157112902 hasAuthorship W2157112902A5036397423 @default.
• W2157112902 hasAuthorship W2157112902A5082250660 @default.
• W2157112902 hasAuthorship W2157112902A5091211694 @default.
• W2157112902 hasConcept C127313418 @default.
• W2157112902 hasConcept C151730666 @default.
• W2157112902 hasConcept C16942324 @default.
• W2157112902 hasConcept C17409809 @default.
• W2157112902 hasConcept C23923706 @default.
• W2157112902 hasConcept C2779870107 @default.
• W2157112902 hasConcept C2780364934 @default.
• W2157112902 hasConcept C34682378 @default.
• W2157112902 hasConcept C4992710 @default.
• W2157112902 hasConcept C51151373 @default.
• W2157112902 hasConcept C58097730 @default.
• W2157112902 hasConcept C67236022 @default.
• W2157112902 hasConcept C77928131 @default.
• W2157112902 hasConcept C79572550 @default.
• W2157112902 hasConcept C84372278 @default.
• W2157112902 hasConcept C93746451 @default.
• W2157112902 hasConceptScore W2157112902C127313418 @default.

• next