FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2053670196> ?p ?o ?g. }

• W2053670196 endingPage "786" @default.
• W2053670196 startingPage "778" @default.
• W2053670196 abstract "The Mersin ophiolite is an ∼6-km-thick oceanic crustal sequence in the central Taurides (southern Turkey), forming large outcrops on the southern flank of Bolkardag. It comprises a sequence of units and includes, in ascending structural order, the Mersin melange, subophiolitic metamorphics, tectonics, ultramafic and mafic cumulates, and pillow lavas interlayered with deep-marine sediments. Thin beds of ophiolite-related metamorphics occupy a constant stratigraphic position at the base of the thick ultramafic unit and include a characteristic rock association of amphibolite and amphibolitic schist, epidote-amphibole schist, quartz-mica schist, calcschist, and marble, which exhibits a typical inverted metamorphic zonation from upper amphibolite to greenschist facies. The protoliths of these metamorphics are oceanic-island basaltic rocks and associated pelagic sediments. They are cut by a swarm of approximately E-W-trending, post-metamorphic, MORB-type tholeiite, microgabbroic-diabasic dikes, which are seen not to affect the structurally overlying harzburgites. The initial detachment of these metamorphics from the oceanic crust during closure of the Neotethyan ocean commenced in the late Cenomanian (96 to 92 Ma, 40Ar/39Ar hornblende ages). The metamorphics have a well-developed migmatitic structure and metamorphic banding defined by alternating epidote-rich and carbonate layers. A pronounced regional foliation (S1), NW-SE-trending mineral lineation (L1), and first-order intrafolial folds (F1) were produced during their deformation. Imbricated structure also is typical in these metamorphics. The meso-structures-such as asymmetry of calcite-augen, vergence and asymmetry of F1 folds, general trend of brittle-ductile structures such as oblique-slip normal and thrust/reverse faults, and vergence of thrusts in the imbricate structure—all indicate unambiguous non-coaxial deformation and a shear sense of upper levels moving up to the NW. The structural evidence suggests that the Mersin ophiolite was obducted over the Bolkardag Mesozoic carbonates from the SE to the NW. The shear sense obtained from the subophiolitic metamorphics is compatible with the general trend and vergence of the large-scale thrust sheets that comprise the Mersin ophiolite." @default.
• W2053670196 created "2016-06-24" @default.
• W2053670196 creator A5024010685 @default.
• W2053670196 creator A5072349202 @default.
• W2053670196 creator A5089404412 @default.
• W2053670196 date "1996-08-01" @default.
• W2053670196 modified "2023-10-01" @default.
• W2053670196 title "The Obduction Direction of the Mersin Ophiolite: Structural Evidence from Subophiolitic Metamorphics in the Central Tauride Belt, Southern Turkey" @default.
• W2053670196 cites W1980767624 @default.
• W2053670196 cites W2025761960 @default.
• W2053670196 cites W2034993532 @default.
• W2053670196 cites W2045745603 @default.
• W2053670196 cites W2049603471 @default.
• W2053670196 cites W2058107818 @default.
• W2053670196 cites W2070588971 @default.
• W2053670196 cites W2076052525 @default.
• W2053670196 cites W2076927877 @default.
• W2053670196 cites W2082157886 @default.
• W2053670196 cites W2084401884 @default.
• W2053670196 cites W2114818838 @default.
• W2053670196 cites W2133994684 @default.
• W2053670196 cites W2134214654 @default.
• W2053670196 cites W2147433838 @default.
• W2053670196 cites W2151792848 @default.
• W2053670196 cites W2161432838 @default.
• W2053670196 cites W2324048702 @default.
• W2053670196 cites W2736726744 @default.
• W2053670196 cites W4254876612 @default.
• W2053670196 cites W642264229 @default.
• W2053670196 doi "https://doi.org/10.1080/00206819709465361" @default.
• W2053670196 hasPublicationYear "1996" @default.
• W2053670196 type Work @default.
• W2053670196 sameAs 2053670196 @default.
• W2053670196 citedByCount "22" @default.
• W2053670196 countsByYear W20536701962014 @default.
• W2053670196 countsByYear W20536701962016 @default.
• W2053670196 countsByYear W20536701962017 @default.
• W2053670196 countsByYear W20536701962018 @default.
• W2053670196 countsByYear W20536701962019 @default.
• W2053670196 countsByYear W20536701962020 @default.
• W2053670196 countsByYear W20536701962021 @default.
• W2053670196 countsByYear W20536701962022 @default.
• W2053670196 crossrefType "journal-article" @default.
• W2053670196 hasAuthorship W2053670196A5024010685 @default.
• W2053670196 hasAuthorship W2053670196A5072349202 @default.
• W2053670196 hasAuthorship W2053670196A5089404412 @default.
• W2053670196 hasConcept C101139013 @default.
• W2053670196 hasConcept C109007969 @default.
• W2053670196 hasConcept C114793014 @default.
• W2053670196 hasConcept C120806208 @default.
• W2053670196 hasConcept C127313418 @default.
• W2053670196 hasConcept C146588470 @default.
• W2053670196 hasConcept C151730666 @default.
• W2053670196 hasConcept C154200439 @default.
• W2053670196 hasConcept C17409809 @default.
• W2053670196 hasConcept C192241223 @default.
• W2053670196 hasConcept C192717286 @default.
• W2053670196 hasConcept C193944797 @default.
• W2053670196 hasConcept C195081551 @default.
• W2053670196 hasConcept C23923706 @default.
• W2053670196 hasConcept C26687426 @default.
• W2053670196 hasConcept C37045145 @default.
• W2053670196 hasConcept C58097730 @default.
• W2053670196 hasConcept C5900021 @default.
• W2053670196 hasConcept C77928131 @default.
• W2053670196 hasConcept C79927612 @default.
• W2053670196 hasConcept C95628711 @default.
• W2053670196 hasConcept C98742433 @default.
• W2053670196 hasConceptScore W2053670196C101139013 @default.
• W2053670196 hasConceptScore W2053670196C109007969 @default.
• W2053670196 hasConceptScore W2053670196C114793014 @default.
• W2053670196 hasConceptScore W2053670196C120806208 @default.
• W2053670196 hasConceptScore W2053670196C127313418 @default.
• W2053670196 hasConceptScore W2053670196C146588470 @default.
• W2053670196 hasConceptScore W2053670196C151730666 @default.
• W2053670196 hasConceptScore W2053670196C154200439 @default.
• W2053670196 hasConceptScore W2053670196C17409809 @default.
• W2053670196 hasConceptScore W2053670196C192241223 @default.
• W2053670196 hasConceptScore W2053670196C192717286 @default.
• W2053670196 hasConceptScore W2053670196C193944797 @default.
• W2053670196 hasConceptScore W2053670196C195081551 @default.
• W2053670196 hasConceptScore W2053670196C23923706 @default.
• W2053670196 hasConceptScore W2053670196C26687426 @default.
• W2053670196 hasConceptScore W2053670196C37045145 @default.
• W2053670196 hasConceptScore W2053670196C58097730 @default.
• W2053670196 hasConceptScore W2053670196C5900021 @default.
• W2053670196 hasConceptScore W2053670196C77928131 @default.
• W2053670196 hasConceptScore W2053670196C79927612 @default.
• W2053670196 hasConceptScore W2053670196C95628711 @default.
• W2053670196 hasConceptScore W2053670196C98742433 @default.
• W2053670196 hasIssue "8" @default.
• W2053670196 hasLocation W20536701961 @default.
• W2053670196 hasOpenAccess W2053670196 @default.
• W2053670196 hasPrimaryLocation W20536701961 @default.
• W2053670196 hasRelatedWork W1487604740 @default.
• W2053670196 hasRelatedWork W1496496489 @default.
• W2053670196 hasRelatedWork W1969092926 @default.
• W2053670196 hasRelatedWork W2053670196 @default.

• next