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Antalya Nappes

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Journal Article
Published: 01 November 2003
Journal of Micropalaeontology (2003) 22 (2): 147–162.
...UGUR KAGAN TEKIN; TUGRUL SUKRU YURTSEVER Abstract The Gökdere Formation of the Alakircay Nappe (Antalya Nappes) mainly consists of cherty limestone and limestone with calciturbidite intercalations. Moderately to well-preserved radiolarians were obtained from the Gökcam section of the Gökdere...
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Journal Article
Published: 07 November 2018
Canadian Journal of Earth Sciences (2019) 56 (11): 1262–1283.
...Nazif Şahin; Demir Altiner Testing of Middle Permian – Lower Triassic stratigraphic data from the Antalya Nappes in a half-graben/tilt-block system has revealed the presence of episodic rifting events separated by periods of tectonic quiescence. Following a period of uplift during the Permian (Late...
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Journal Article
Published: 01 July 2008
Bulletin de la Société Géologique de France (2008) 179 (4): 397–410.
... unit of the Middle Antalya nappes, southwestern Turkey. New determinations on conodont faunas allow to date this sequence to the Lower Carnian (Julian). The volcanic rocks show rather homogeneous compositions, with high TiO 2 and relatively low MgO and Ni contents which suggest olivine fractionation...
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Journal Article
Published: 01 January 2004
Micropaleontology (2004) 50 (3): 281–295.
...Sylvie Crasquin-Soleau; Jean Marcoux; Lucia Angiolini; Sylvain Richoz; Alda Nicora; Aymon Baud; Yann Bertho Abstract The Permian - Triassic boundary of the Çürük dađ section (Taurus, Antalya Nappes, Turkey) was sampled for ostracodes. 38 species belonging to 22 genera were discovered...
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Journal Article
Published: 01 April 2002
Micropaleontology (2002) 48 (2): 177–205.
...Ugur Kagan Tekin Abstract The Hocakoy section, measured in the Alakircay Nappe of Antalya Nappes in SW Turkey, is one of the key sections that contains Upper Triassic to Middle Cretaceous Radiolaria bearing pelagic sediments. The lower part of the section is the Upper Triassic Gokdere Formation...
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Structural sketch map of the sampled area (Kara Dere unit, <span class="search-highlight">Antalya</span> <span class="search-highlight">Nappes</span>, ...
Published: 01 July 2008
F ig . 2. – Structural sketch map of the sampled area (Kara Dere unit, Antalya Nappes, SW Turkey), and position of the studied samples. F ig . 2. – Carte structurale schématique de la zone étudiée (unité de Kara Dere, nappes d’Antalya, Turquie du SW), et position des échantillons
Journal Article
Published: 01 November 2007
Proceedings of the Yorkshire Geological Society (2007) 56 (4): 261–265.
... Mountains, rocks of the Gagae area belong to the Antalya Nappes and are succeeded by a Cretaceous ophiolitic unit. Associated dark volcanic rocks are not considered compatible with those for which Pliny's term was originally employed, and interbedded, organic-rich, black layers in the Alakir Çay Unit, one...
FIGURES
Journal Article
Published: 01 March 2011
Bulletin de la Société Géologique de France (2011) 182 (2): 133–148.
...André Poisson; Fabienne Orszag-Sperber; Erdal Kosun; Maria-Angella Bassetti; Carla Müller; Roland Wernli; Jean-Marie Rouchy Abstract The Mio-Pliocene basins around the Antalya gulf in SW Turkey developed above the Tauric Mesozoic platforms on which the Antalya nappes had been thrusted (in Late...
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Series: Geological Society, London, Special Publications
Published: 01 January 2000
DOI: 10.1144/GSL.SP.2000.173.01.14
EISBN: 9781862394216
...-authocthonous carbonate platform overthrust by the Antalya Nappes and Alanya Massif metamorphics. The sedimentary fill is represented by clasticdominated deposits consisting of, in ascending order, a conglomeratic wedge, reefal shelf carbonates, limy mudstones, and calciturbidites with subordinate breccias...
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Journal Article
Journal: Geology
Published: 01 September 1986
Geology (1986) 14 (9): 734–737.
...Yves Lagabrielle; Hubert Whitechurch; Jean Marcoux; Thierry Juteau; Ingrid Reuber; François Guillocheau; Ussal Çapan Abstract The ophiolites of the Antalya nappes, cropping out in the area of Kemer (southwestern Turkey), are capped by a spectacular detrital sequence composed of various ophiolitic...
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Major tectonic units of the western part of the <span class="search-highlight">Antalya</span> Gulf. Key: a, Beyda...
Published: 01 November 2003
Fig. 1. Major tectonic units of the western part of the Antalya Gulf. Key: a, Beydaglari Autochthonous Unit; b–e, Antalya Nappes – b, Cataltepe Nappe; c, Alakircay Nappe; d, Tahtalidag Nappe; e, Tekirova Ophiolite Nappe including ophiolitic melange; f, post-Lower Miocene units (revised after
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( A ) Generalized columnar section of the Alakircay <span class="search-highlight">Nappe</span> of the <span class="search-highlight">Antalya</span> Na...
Published: 01 November 2003
Fig. 3. ( A ) Generalized columnar section of the Alakircay Nappe of the Antalya Nappes in the study area (not to scale). ( B ) Gökcam section. Key: a, breccia and conglomerate; b, sandstone; c, shale; d, calciturbidite; e, limestone; f, limestone and chert alternations; g, limestone with chert
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Stratigraphic distributions of dagmaritin foraminifera in the Changhsingian...
Published: 31 January 2021
Figure 7. Stratigraphic distributions of dagmaritin foraminifera in the Changhsingian sections of the Antalya Nappes. Stratigraphic columns are illustrated in Figure 3 .
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Testing of the Middle Permian – Lower Triassic stratigraphic data from the ...
Published: 07 November 2018
Fig. 15. Testing of the Middle Permian – Lower Triassic stratigraphic data from the Antalya Nappes in a half-graben/tilt-block system. [Colour online.]
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Geological map of the Gökcam section and its surroundings. Key: a, undiffer...
Published: 01 November 2003
Fig. 2. Geological map of the Gökcam section and its surroundings. Key: a, undifferentiated Alakircay Nappe of the Antalya Nappes; b, Quaternary deposits; c, Quaternary slope debris; d, drainage systems; e, main roads; f, location of the section (revised after Senel, 1997b).
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Interpretative W-E transversal cross section through the central part of th...
Published: 01 March 2011
on each side by two systems of converging nappes: the Antalya nappes to the east (age of the thrust: Late Cretaceous-Paleocene, reactivated in the Late Miocene - mid Pliocene times), and the Lycian nappes (age of the thrust: Langhian). Two deep wells give data for the interpretation of the deep structure
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Simplified geological map showing the main tectonic belts of the western Ta...
Published: 01 July 2006
F igure 1. Simplified geological map showing the main tectonic belts of the western Taurides (after Poisson and others, 1983 ). a) Tertiary-Quaternary formations, b) Bey Dağları autochthon, c) Antalya nappes, d) Lycian nappes, e) Section locations of previous researchers. Also shown
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Major, trace element and isotopic (Nd, Sr, Pb) analyses of the Late Triassi...
Published: 01 July 2008
T able III. – Major, trace element and isotopic (Nd, Sr, Pb) analyses of the Late Triassic alkaline volcanic rocks from Antalya Nappes. Total iron as Fe 2 O 3 . Sums of major element oxides recalculated to 100 %. For a given sample, the first column of major and trace element data corresponds
Journal Article
Published: 31 January 2021
Journal of Foraminiferal Research (2021) 51 (1): 14–31.
...Figure 7. Stratigraphic distributions of dagmaritin foraminifera in the Changhsingian sections of the Antalya Nappes. Stratigraphic columns are illustrated in Figure 3 . ...
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Journal Article
Published: 01 October 2010
Clays and Clay Minerals (2010) 58 (5): 644–666.
...) of the Antalya Unit include different rock units with respect to age and tectonic setting (Figure 2 ). In the study area, the Tahtalıdağ nappe is dominated by steeply dipping slices of Paleozoic (Cambrian to Permian) sedimentary rocks. The lowermost parts of the Tahtalıdağ nappe comprise Middle Cambrian...
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