FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2261569593> ?p ?o ?g. }

• W2261569593 abstract "Abstract The South Dehshir Ophiolite, exposed along the southwestern margin of the Central Iranian microcontinent, comprises a mantle and a crustal sequence. This massif contains serpentinized peridotites, gabbros and diabase sheeted dykes cutting across wherlite, pegmatitic gabbro and plagiogranite, and is tectonically covered by radiolarites, pelagic limestones with Late Cretaceous microfauna and lavas. Under a microscope, the gabbros exhibit mesocumulate, adcumulate and hetradcumulate textures presumably formed in open magma chambers. Hypabyssal and lava samples show tholeiitic to calc-alkaline affinities, and their compositions cluster in the fields of arc or supra-subduction zone magmatism. Binary diagrams display compositional trends of magmatic differentiation, plotting away from the mid-ocean-ridge basalt (MORB) (tholeiitic) trend and following the arc (calc-alkaline) trend. Rare Earth element (REE) and spider diagrams display various enrichments at different levels. Moderate enrichment of the large-ion lithophile elements (LILE; Rb, Ba, Th, U, La, Sr) relative to the high-field-strength elements (HFSE; Nb, Ta) and slight depletion of Ti and Zr in some patterns may be attributed to variable influences of subduction components over the depleted mantle wedge. Elemental ratios display evidence for the contribution of both fluids and melt released from the subducted slab. Few patterns display ocean-island basalt (OIB) characteristics, possibly attributed to the involvement of local mantle plumes on the partial melting of the mantle wedge. This evidence indicates that the crustal rocks of the South Dehshir Ophiolite formed in a supra-subduction zone." @default.
• W2261569593 created "2016-06-24" @default.
• W2261569593 creator A5016894052 @default.
• W2261569593 creator A5021445006 @default.
• W2261569593 creator A5044941615 @default.
• W2261569593 date "2015-10-07" @default.
• W2261569593 modified "2023-09-27" @default.
• W2261569593 title "Tectonomagmatic evolution of the South Dehshir Ophiolite, Central Iran" @default.
• W2261569593 cites W1517626857 @default.
• W2261569593 cites W1557600004 @default.
• W2261569593 cites W1566514932 @default.
• W2261569593 cites W161156827 @default.
• W2261569593 cites W1837708467 @default.
• W2261569593 cites W1963794532 @default.
• W2261569593 cites W1964909252 @default.
• W2261569593 cites W1965596457 @default.
• W2261569593 cites W1974505893 @default.
• W2261569593 cites W1986518408 @default.
• W2261569593 cites W1991363467 @default.
• W2261569593 cites W1992736932 @default.
• W2261569593 cites W1994748013 @default.
• W2261569593 cites W2001055470 @default.
• W2261569593 cites W2013491092 @default.
• W2261569593 cites W2014832120 @default.
• W2261569593 cites W2020818305 @default.
• W2261569593 cites W2022865240 @default.
• W2261569593 cites W2026699431 @default.
• W2261569593 cites W2029622065 @default.
• W2261569593 cites W2030254360 @default.
• W2261569593 cites W2031295342 @default.
• W2261569593 cites W2042700532 @default.
• W2261569593 cites W2044938578 @default.
• W2261569593 cites W2046018899 @default.
• W2261569593 cites W2047519592 @default.
• W2261569593 cites W2047965201 @default.
• W2261569593 cites W2072248712 @default.
• W2261569593 cites W2077577717 @default.
• W2261569593 cites W2078673459 @default.
• W2261569593 cites W2083396877 @default.
• W2261569593 cites W2086424708 @default.
• W2261569593 cites W2087939324 @default.
• W2261569593 cites W2101320847 @default.
• W2261569593 cites W2121368895 @default.
• W2261569593 cites W2137159697 @default.
• W2261569593 cites W2139788788 @default.
• W2261569593 cites W2144461623 @default.
• W2261569593 cites W2155252883 @default.
• W2261569593 cites W2157099954 @default.
• W2261569593 cites W2160943613 @default.
• W2261569593 cites W2161188118 @default.
• W2261569593 cites W2164064321 @default.
• W2261569593 cites W2165094726 @default.
• W2261569593 cites W2313567947 @default.
• W2261569593 cites W2316957776 @default.
• W2261569593 cites W2332471046 @default.
• W2261569593 cites W4254941784 @default.
• W2261569593 cites W642264229 @default.
• W2261569593 doi "https://doi.org/10.1017/s0016756815000618" @default.
• W2261569593 hasPublicationYear "2015" @default.
• W2261569593 type Work @default.
• W2261569593 sameAs 2261569593 @default.
• W2261569593 citedByCount "2" @default.
• W2261569593 countsByYear W22615695932018 @default.
• W2261569593 countsByYear W22615695932020 @default.
• W2261569593 crossrefType "journal-article" @default.
• W2261569593 hasAuthorship W2261569593A5016894052 @default.
• W2261569593 hasAuthorship W2261569593A5021445006 @default.
• W2261569593 hasAuthorship W2261569593A5044941615 @default.
• W2261569593 hasConcept C120806208 @default.
• W2261569593 hasConcept C127313418 @default.
• W2261569593 hasConcept C151730666 @default.
• W2261569593 hasConcept C161509811 @default.
• W2261569593 hasConcept C17409809 @default.
• W2261569593 hasConcept C192241223 @default.
• W2261569593 hasConcept C193944797 @default.
• W2261569593 hasConcept C23923706 @default.
• W2261569593 hasConcept C2780040746 @default.
• W2261569593 hasConcept C58097730 @default.
• W2261569593 hasConcept C5900021 @default.
• W2261569593 hasConcept C67236022 @default.
• W2261569593 hasConcept C73462661 @default.
• W2261569593 hasConcept C77928131 @default.
• W2261569593 hasConcept C79572550 @default.
• W2261569593 hasConcept C79605941 @default.
• W2261569593 hasConcept C83948199 @default.
• W2261569593 hasConceptScore W2261569593C120806208 @default.
• W2261569593 hasConceptScore W2261569593C127313418 @default.
• W2261569593 hasConceptScore W2261569593C151730666 @default.
• W2261569593 hasConceptScore W2261569593C161509811 @default.
• W2261569593 hasConceptScore W2261569593C17409809 @default.
• W2261569593 hasConceptScore W2261569593C192241223 @default.
• W2261569593 hasConceptScore W2261569593C193944797 @default.
• W2261569593 hasConceptScore W2261569593C23923706 @default.
• W2261569593 hasConceptScore W2261569593C2780040746 @default.
• W2261569593 hasConceptScore W2261569593C58097730 @default.
• W2261569593 hasConceptScore W2261569593C5900021 @default.
• W2261569593 hasConceptScore W2261569593C67236022 @default.
• W2261569593 hasConceptScore W2261569593C73462661 @default.
• W2261569593 hasConceptScore W2261569593C77928131 @default.
• W2261569593 hasConceptScore W2261569593C79572550 @default.

• next