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- W4200593958 endingPage "1190" @default.
- W4200593958 startingPage "1139" @default.
- W4200593958 abstract "The Aladağ melange is located between Mesozoic Tauride carbonate platform units and the Late Cretaceous Pozantı-Karsantı ophiolite and its metamorphic sole. The melange comprises a lower, mainly sedimentary unit, composed of variably disrupted thrust sheets of deep-sea sediments, with a localized matrix of mass-flow and turbidity current deposits. The upper, volcanic-sedimentary melange comprises highly disrupted basalt-pelagic carbonate-radiolarite units, rarely associated with gravity-flow deposits. Tholeiitic to alkaline basalts in the melange range from N-MORB, to E-MORB and to OIB, and are dated as Middle Jurassic to Early Cretaceous using Radiolaria from interbedded pelagic sediments. Comparisons with accretionary melanges throughout southern Turkey and elsewhere indicate a similar geochemical pattern of variable ‘enrichment’, commonly coupled with a subduction influence (e.g. negative Nb, Ta anomalies). Geochemically, the subduction-influenced basalts are consistent with an oceanic island arc origin. However, the geological setting of Triassic basalts within some of the melanges (e.g. Mersin) is indicative of a rifted continental margin setting. The Mesozoic basalts within the Turkish melanges considered here erupted along the distal, outer northern margin of the Tauride continent, followed by Late Cretaceous subduction-accretion and supra-subduction zone ophiolite emplacement. Regional to global chemical comparisons suggest that the subduction influence could represent geochemical subduction inheritance rather than contemporaneous subduction." @default.
- W4200593958 created "2021-12-31" @default.
- W4200593958 creator A5000901892 @default.
- W4200593958 creator A5037828119 @default.
- W4200593958 creator A5089404412 @default.
- W4200593958 date "2021-12-05" @default.
- W4200593958 modified "2023-10-17" @default.
- W4200593958 title "Role of Late Cretaceous volcanic-sedimentary melanges, specifically the Aladağ melange, E Turkey, in the rift-drift-subduction-accretion-emplacement history of the Tethyan Inner Tauride ocean" @default.
- W4200593958 cites W127965863 @default.
- W4200593958 cites W1477432882 @default.
- W4200593958 cites W1529124630 @default.
- W4200593958 cites W1964577448 @default.
- W4200593958 cites W1964977415 @default.
- W4200593958 cites W1966934203 @default.
- W4200593958 cites W1969021229 @default.
- W4200593958 cites W1972835127 @default.
- W4200593958 cites W1979002031 @default.
- W4200593958 cites W1979170550 @default.
- W4200593958 cites W1979399178 @default.
- W4200593958 cites W1979427870 @default.
- W4200593958 cites W1979542320 @default.
- W4200593958 cites W1987060841 @default.
- W4200593958 cites W1988251519 @default.
- W4200593958 cites W1992069730 @default.
- W4200593958 cites W1994266650 @default.
- W4200593958 cites W1994935654 @default.
- W4200593958 cites W1997468419 @default.
- W4200593958 cites W2003419738 @default.
- W4200593958 cites W2003622214 @default.
- W4200593958 cites W2004027243 @default.
- W4200593958 cites W2005072945 @default.
- W4200593958 cites W2007245030 @default.
- W4200593958 cites W2007700279 @default.
- W4200593958 cites W2008212652 @default.
- W4200593958 cites W2009538935 @default.
- W4200593958 cites W2012625291 @default.
- W4200593958 cites W2012746911 @default.
- W4200593958 cites W2013259970 @default.
- W4200593958 cites W2015577392 @default.
- W4200593958 cites W2017046678 @default.
- W4200593958 cites W2017343540 @default.
- W4200593958 cites W2018946474 @default.
- W4200593958 cites W2027742206 @default.
- W4200593958 cites W2028446118 @default.
- W4200593958 cites W2029548885 @default.
- W4200593958 cites W2031295342 @default.
- W4200593958 cites W2033085520 @default.
- W4200593958 cites W2033716240 @default.
- W4200593958 cites W2034333474 @default.
- W4200593958 cites W2034499697 @default.
- W4200593958 cites W2034993532 @default.
- W4200593958 cites W2038987825 @default.
- W4200593958 cites W2039609381 @default.
- W4200593958 cites W2045567035 @default.
- W4200593958 cites W2045594539 @default.
- W4200593958 cites W2045745603 @default.
- W4200593958 cites W2046078416 @default.
- W4200593958 cites W2046241309 @default.
- W4200593958 cites W2046696482 @default.
- W4200593958 cites W2046869706 @default.
- W4200593958 cites W2046958094 @default.
- W4200593958 cites W2052600810 @default.
- W4200593958 cites W2053670196 @default.
- W4200593958 cites W2064834605 @default.
- W4200593958 cites W2066968708 @default.
- W4200593958 cites W2067566353 @default.
- W4200593958 cites W2068921463 @default.
- W4200593958 cites W2069158492 @default.
- W4200593958 cites W2070588971 @default.
- W4200593958 cites W2071030838 @default.
- W4200593958 cites W2071538549 @default.
- W4200593958 cites W2072422667 @default.
- W4200593958 cites W2073724397 @default.
- W4200593958 cites W2075151941 @default.
- W4200593958 cites W2075994346 @default.
- W4200593958 cites W2077475173 @default.
- W4200593958 cites W2079134540 @default.
- W4200593958 cites W2079891283 @default.
- W4200593958 cites W2080224624 @default.
- W4200593958 cites W2084150033 @default.
- W4200593958 cites W2089068201 @default.
- W4200593958 cites W2089645958 @default.
- W4200593958 cites W2095601024 @default.
- W4200593958 cites W2096168179 @default.
- W4200593958 cites W2096297752 @default.
- W4200593958 cites W2099024625 @default.
- W4200593958 cites W2108056426 @default.
- W4200593958 cites W2108220699 @default.
- W4200593958 cites W2108884538 @default.
- W4200593958 cites W2113480398 @default.
- W4200593958 cites W2114676111 @default.
- W4200593958 cites W2115460911 @default.
- W4200593958 cites W2115550380 @default.
- W4200593958 cites W2117094294 @default.
- W4200593958 cites W2119524910 @default.
- W4200593958 cites W2123794117 @default.
- W4200593958 cites W2124496839 @default.
- W4200593958 cites W2127485798 @default.