Results 1 to 10 of about 17,905 (130)
Lithostratigraphy and planktonic foraminifera of the uppermost Cretaceous-Upper Paleocene strata of the Tavas nappe of the Lycian nappes (SW Turkey) [PDF]
Geologia Croatica, 2017 The Lycian nappes lying on top of the para–autochthonous metamorphosed Menderes and unmetamorphosed Bey Dağları successions in SW Anatolia belong to the Tauride segment of the Anatolide–Tauride Block.
Bilal Sari
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Late Triassic ostracods from the Lycian Nappes, southwestern Turkey: implications on taxonomy and palaeobiogeographical distribution [PDF]
BSGF - Earth Sciences Bulletin, 2020 The first ostracods known from the Lycian Nappes in southwestern Turkey are here reported, adding to the scientific understanding of marine ostracods during the Cordevolian, early Carnian, Late Triassic.
Forel Marie-Béatrice, Moix Patrice
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Geologia Croatica, 2010 For the first time. a deep-water Lower Carbon iferous siliciclasticturbidite-olistostrome unit with many lydites (partly distally turbiditic) can be dated in the Incirbeleni Formation of the Tavas Nappe (Lycian nappes) in southwestern Turkey.
Heinz W. Kozur +2 more
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Deformation history of the high‐pressure Lycian Nappes and implications for tectonic evolution of SW Turkey [PDF]
Tectonics, 2003 In southwestern Turkey, the Lycian nappe complex which overlies the autochthonous Menderes Massif and Bey Dağ platform, consists from base to top of metasediments, a mélange unit and an ophiolitic sequence. Fresh Fe‐Mg‐carpholite occurrence in the metasediments attests to a high‐pressure low‐temperature metamorphic event.
Gaëtan Rimmelé +3 more
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International Geology Review, 2018 In the eastern Mediterranean, the Lycian Nappes are found in the structurally uppermost position in the Anatolide-Tauride belt related to the closure of the Neotethys. In Western Turkey, the Marmaris Ophiolite with the metamorphic sole occupies the uppermost tectonic position in the Lycian belt.
Gungor, Talip +5 more
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Cretaceous Research, 2017 Abstract Lycian Nappes (in SW Turkey) lie between the Menderes Massif and Bey Daglari carbonates and comprise thrust sheets (nappes piles) of Paleozoic-Cenozoic rocks, ophiolitic and tectonic melanges and serpentinized peridodites. This study focuses on identification of rudists and their palaeoenvironmental features observed within the Cretaceous ...
Ozer, Sacit +5 more
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Cretaceous Research, 2015 Abstract Megablocks of coral-rudist bearing platform limestone, of Stramberk type, are present as exotics in upper Santonian–Campanian flysch-like deposits of the Karabortlen formation, near Bodrum. These beds belong to the Lycian nappes and the palaeogeographic origin of the megablocks is unclear.
Masse, Jean-Pierre +4 more
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Bulletin de la Société Géologique de France, 2004 Abstract The recent discovery of HP-LT parageneses in the basal unit of the Lycian nappes and in the Mesozoic cover of the Menderes massif leads us to reconsider and discuss the correlation of this region with the nearby collapsed Helle-nides in the Aegean domain.
Jolivet, Laurent +4 more
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Paleoseismological features and tectonic setting of the Fethiye-Burdur fault zone (SW Turkey) [PDF]
Geološki Anali Balkanskoga Poluostrva, 2023 The Fethiye‐Burdur fault zone is not a single line. Still, it consists of discontinuous northeasterly trending fault segments developed parallel to each other between the Gulf of Fethiye and Burdur Lake.
Sari Coşkun +5 more
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The structure of the Palaeozoic schists in the Southern Menderes Massif, western Turkey: a new approach to the origin of the Main Menderes Metamorphism and its relation to the Lycian Nappes [PDF]
Geodinamica Acta, 1999 Erdin Bozkurt, R. Graham Park
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