Results 61 to 70 of about 239 (95)
International Geology Review, 2019 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.
Talip Güngör, Cuneyt Akal
exaly +5 more sources
International Journal of Earth Sciences, 2001 In the basal thrust sheets of the Lycian nappes fresh Fe-Mg-carpholite documents low-grade. high-pressure (HP) metamorphism. Here we describe the first occurrences of this HP indicator mineral in Turkey, its regional distribution and geodynamic ...
R Oberhänsli +2 more
exaly +5 more sources
Bulletin - Societie Geologique De France, 2004 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 Hellenides in the Aegean domain.
Laurent Jolivet +2 more
exaly +7 more sources
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 The Early Eocene to Early Oligocene tectonic history of the Menderes Massif involves a major regional Barrovian-type metamorphism (M-1, Main Menderes Metamorphism, MMM), present only in the Palaeozoic-Cenozoic metasediments (the so-called "cover" of the ...
Erdin Bozkurt
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Cretaceous Research, 2015 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.
Jean-Pierre Masse +1 more
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Journal of Geology, 2015 The Turunc Unit, which represents one of the tectonic slices within the Lycian Nappes in southwestern Anatolia, preserves the remnants derived from the northern branch of Neotethys. The unit includes basalts intercalated with pelagic limestones of middle
M Cemal Göncüoğlu, U Kagan Tekin
exaly +4 more sources
Oligo-Miocene extension in the Lycian orogen: evidence from the Lycian molasse basin, SW Turkey
Geodinamica Acta, 2005 The Lycian molasse basin of SW Turkey is a NE-SW-oriented basin that developed on an imbricated basement, comprising the allochthonous Mesozoic rocks of the Lycian nappes and Palaeocene-Eocene supra-allochthonous sediments.
Hasan Sözbilir
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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.
Laurent Jolivet +2 more
exaly +2 more sources
Geological Society Special Publication, 2006 In SW Turkey, Fe-Mg-carpholite has recently been recognized in the basal metasediments of the Lycian Nappes, which overthrust the Menderes Massif on its southern flank. This high-pressure-low-temperature (HP-LT) metamorphic index mineral was widely found
Roland Oberhänsli +2 more
exaly +2 more sources
Some of the next articles are maybe not open access.
Kubergandian (Roadian, Middle Permian) of the Lycian and Aladağ Nappes (Southern Turkey)
Geobios, 2013Abstract The Nisangahtepe Formation (Teke Dere unit) in the Lycian Nappes, and reworked pebbles and blocks from the Late Triassic Gevne Formation in the Aladag unit (both in Southern Turkey), present a well-developed Kubergandian microfauna and microflora found for the first time in this area.
Daniel Vachard
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