Results 71 to 80 of about 239 (95)
Journal of Petrology, 2005 The Menderes Massif and the overlying Lycian Nappes occupy an extensive area of SW Turkey where high-pressure- low-temperature metamorphic rocks occur.
Teddy PARRA +2 more
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Revue De Micropaleontologie, 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
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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
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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.
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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.
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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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Mesoscopic and microscopic structures along the contact between Menderes massif and Lycian nappes
2021ÖZET Milas bölgesinde Menderes Masifinin güney kesimi ile Likya Naplannın batı kesimi yüzlek verir. Likya Naplan ince serpantinit dilimlerinin bulunduğu, güneye eğimli, düşük açılı tektonik bir dokanak boyunca Menderes Masifini üstlemektedir. Neojen yaşlı karasal tortullar bu iki tektonik kuşağa ait kayaları açısal uyumsuz bir dokanak boyunca örter ...
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FORMATION OF PODIFORM DUNITES IN THE LYCIAN PERIDOTITE NAPPES (AGLA - KOYCEGIZ, SW TURKEY)
2009In this study, the whole-rock major oxides, trace elements and mineral chemistry of the Agla peridotites (comprising host harzburgites and podiform dunites) are investigated to determine the formation mechanisms of the Agla podiform dunites (SW Turkey).
Gnos, Edwin +4 more
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Geology of the Menderes Massif and the Lycian Nappes South of Denizli, Western Taurides
1987Mount Honaz region in the Western Taurides is made up of superimposed several tectonic units. In the west, monotonous green metashales called the Honaz shale occur at the base of the tectonic stack. Honaz shale is tectonically overlain by weakly metamorphosed, massif white limestone, thinly bedded cherty limestone and shale which covers the Mendercs ...
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The extension of the Lycian Nappes (SW Turkey) into the Southeastern Aegean Islands
1974Bernoulli, Daniel +2 more
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Emplacement age and direction of the Lycian nappes in the Söke-Selçuk region, western Turkey
International Journal of Earth Sciences, 2001Talip Güngör
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