Results 91 to 100 of about 17,905 (130)
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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, Patrice Moix
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Mineralogical Magazine, 1984
AbstractIn the Ören area at the base of the Lycian Nappes, chloritoid is common on a regional scale. Mn and inferred Fe3+contents are low. Chloritoid + quartz occur rather than the more hydrous equivalent pyrophyllite + chlorite, Fe/(Fe + Mg) values in chlorite ranging down to 0·27.
J. R. Ashworth, M. M. Evirgen
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AbstractIn the Ören area at the base of the Lycian Nappes, chloritoid is common on a regional scale. Mn and inferred Fe3+contents are low. Chloritoid + quartz occur rather than the more hydrous equivalent pyrophyllite + chlorite, Fe/(Fe + Mg) values in chlorite ranging down to 0·27.
J. R. Ashworth, M. M. Evirgen
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Geological Society, London, Special Publications, 1984
Summary The western Tauride Mountains of S.W. Turkey comprise a central relatively autochthonous carbonate platform unit, the Tauride autochthon bordered by two allochthonous units, the Lycian Nappes to the west and the Antalya Complex to the east.
A. B. Hayward
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Summary The western Tauride Mountains of S.W. Turkey comprise a central relatively autochthonous carbonate platform unit, the Tauride autochthon bordered by two allochthonous units, the Lycian Nappes to the west and the Antalya Complex to the east.
A. B. Hayward
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Journal of Asian Earth Sciences, 2013
Abstract The orientation, asymmetry and cross-cutting relationships of the structures along the contact zone between the Lycian nappes and the Menderes Massif suggest the presence of three deformation phases in the Milas region of southwest Turkey. The first deformation phase (D1) is characterized by a ductile deformation with top-to-the-NE sense of ...
Passchier, Cees W. +3 more
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Abstract The orientation, asymmetry and cross-cutting relationships of the structures along the contact zone between the Lycian nappes and the Menderes Massif suggest the presence of three deformation phases in the Milas region of southwest Turkey. The first deformation phase (D1) is characterized by a ductile deformation with top-to-the-NE sense of ...
Passchier, Cees W. +3 more
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The Journal of Geology, 2015
AbstractThe 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 Carnian age (early Late Triassic) based on the characteristic radiolarian assemblage of the
Sayıt, Kaan +2 more
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AbstractThe 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 Carnian age (early Late Triassic) based on the characteristic radiolarian assemblage of the
Sayıt, Kaan +2 more
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Journal of Geochemical Exploration, 2003
Abstract Associated with the emplacement of the Lycian nappes, SW Turkey, Cretaceous limestones were thrusted over an ophiolitic melange in their front zone. Miocene flysch formed immediately in front of these nappes and were overthrusted by the Lycian nappes.
Philippe Muchez +4 more
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Abstract Associated with the emplacement of the Lycian nappes, SW Turkey, Cretaceous limestones were thrusted over an ophiolitic melange in their front zone. Miocene flysch formed immediately in front of these nappes and were overthrusted by the Lycian nappes.
Philippe Muchez +4 more
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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 consequences. Carpholite and its breakdown products, such as chloritiod and pyrophyllite, occur in the Lycian
Oberhänsli, Roland (Prof. Dr.) +3 more
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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 consequences. Carpholite and its breakdown products, such as chloritiod and pyrophyllite, occur in the Lycian
Oberhänsli, Roland (Prof. Dr.) +3 more
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Journal of Asian Earth Sciences, 2015
Abstract Stratigraphic sections (Kizilca and Kizilca North) in the Tavas nappe, western Taurides, Turkey records the event of carbonate platform drowning in the western Tethyan realm. Our detailed biostratigraphic study of radiolarians and other microfossils places the important temporal constraints on this event and indicates that drowning occured ...
Havva Soycan +2 more
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Abstract Stratigraphic sections (Kizilca and Kizilca North) in the Tavas nappe, western Taurides, Turkey records the event of carbonate platform drowning in the western Tethyan realm. Our detailed biostratigraphic study of radiolarians and other microfossils places the important temporal constraints on this event and indicates that drowning occured ...
Havva Soycan +2 more
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Revue de Micropaléontologie, 2011
Abstract Shallow-marine limestones associated to a Palaeotethyan seamount in the Teke Dere unit of the Tavas Nappe (Lycian Nappes, SW Turkey) are essentially latest Moscovian-Kasimovian in age. The wide range of microfauna and -flora of the series show biogeographic affinities comparable to those from the northern Palaeotethyan borders (especially to
Daniel Vachard, Patrice Moix
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Abstract Shallow-marine limestones associated to a Palaeotethyan seamount in the Teke Dere unit of the Tavas Nappe (Lycian Nappes, SW Turkey) are essentially latest Moscovian-Kasimovian in age. The wide range of microfauna and -flora of the series show biogeographic affinities comparable to those from the northern Palaeotethyan borders (especially to
Daniel Vachard, Patrice Moix
openaire +2 more sources