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- W2000822934 abstract "Devonian radiolarian ribbon cherts are found as olistoliths and as a thin (<100 m) tectonic slice in pervasively deformed sandstone and shale in a Triassic subduction-accretion complex (Upper Karakaya Complex) in Northwest Turkey. The subduction-accretion complex also comprises exotic blocks of Lower Carboniferous and Upper Permian limestone. It lies tectonically over a thick metabasite series and is unconformably overlain by little deformed continental to shallow marine sedimentary rocks of Jurassic age. The Devonian radiolarian cherts, along with the earlier descriptions of Carboniferous and Permian radiolarian cherts from the Karakaya Complex suggest the subduction of a Late Paleozoic ocean, the Paleo-Tethys, along the southern margin of the Pontides. Des cherts rubanés dévoniens à radiolaires ont été trouvés sous la forme d’olistolithes et de minces lames tectoniques (<100 m), dans des grès et argiles considérablement déformés d’un complexe de subduction-accrétion triasique (Complexe de Karakaya supérieur) de Turquie nord-occidentale, le complexe de subduction-accrétion comporte aussi des blocs exotiques de calcaire du Carbonifère inférieur et du Permien supérieur. Il repose tectoniquement sur une série épaisse de métabasite et est recouvert en discordance par des roches sédimentaires d’âge Jurassique peu déformées, d’origine continentale à marine peu profonde. Les cherts dévoniens à radiolaires, de même que les descriptions plus récentes de cherts à radiolaires carbonifères et permiens du complexe de Karakaya suggèrent la subduction d’un océan Paléozoïque tardif, la Paléo-Téthys, le long de la marge méridionale des Pontides." @default.
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- W2000822934 date "2011-01-01" @default.
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- W2000822934 title "Devonian radiolarian ribbon cherts from the Karakaya Complex, Northwest Turkey: Implications for the Paleo-Tethyan evolution" @default.
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