Results 121 to 130 of about 1,426 (164)
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Complete Alpine reworking of the northern Menderes Massif, western Turkey
International Journal of Earth Sciences, 2015This study focuses on the petrology, geochronology and thermochronology of metamorphic rocks within the northern Menderes Massif in western Turkey. Metasediments belonging to the cover series of the Massif record pervasive amphibolite-facies metamorphism culminating at ca. 625–670 °C and 7–9 kbars.
Cenki-Tok, Benedicte +5 more
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Cenozoic pure-shear collapse of the southern Menderes Massif, Turkey
Geological Society, London, Special Publications, 2013Abstract A transition from construction to collapse of the Alpine orogen in Middle to Late Eocene time is recorded in the structural fabrics of gneissic rocks in the southern Menderes Massif, western Turkey. Augen gneiss in the southern Menderes Massif indicates a spatial switch of shear sense along a north–south section through ...
Lindsay J. Iredale +2 more
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Journal of the Geological Society, 1999
Based on lithostratigraphic comparisons the Menderes Massif has been correlated with the Cycladic Massif, thereby implying that the eastern Mediterranean consists of a narrow pre-Alpine basement belt which is laterally continuous over a long distance and which experienced a similar Alpine orogenic history.
Ring, U +3 more
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Based on lithostratigraphic comparisons the Menderes Massif has been correlated with the Cycladic Massif, thereby implying that the eastern Mediterranean consists of a narrow pre-Alpine basement belt which is laterally continuous over a long distance and which experienced a similar Alpine orogenic history.
Ring, U +3 more
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Mass and stress changes in the Menderes Massif (Western Anatolia, Turkey)
Journal of Asian Earth Sciences, 2016Abstract Comparing the results of the microgravity and GNSS measurements is useful for understanding the vertical displacements of the plates. In this study, for determining the geodynamical behaviors of seismically active tectonic structures of Gediz and Buyuk Menderes grabens which are located in Western Anatolia (Turkey) graben system, the mass ...
Çırmık, Ayça +2 more
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Menderes Massif (Western Turkey): structural, metamorphic and magmatic evolution - a synthesis
International Journal of Earth Sciences, 2001The Menderes Massif covers large areas in western Turkey. The better understanding of its tectono-metamorphic history would provide insight for the Alpine evolution of western Turkey and the entire eastern Mediterranean region. This paper summarizes the available literature on the metamorphic rocks of western Turkey and that of the Menderes Massif with
Erdin Bozkurt, Roland Oberhänsli
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The Origin of gneisses in the Çine submassif ( Menderes massif )
2021ABSTRACT The study area is located at south of the city of Aydm in the Çine Submassif in the Menderes Massif covers an area, 2 of approximately 190 km. In ascending order, the rock sucression of the region is given as follows: metamorphic basement belonging to the Menderes Massif and Neogene terrestrial sediments covering the basement discordantly. The
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The Menderes massif and the surrounding Caledonian structures
2014Please click the pdf for the full text.
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K-feldspar bearing pegmatities of Çine (Aydın) area, Menderes massif
2021rv ABSTRACT The study area is located in the NE of Çine (Aydın) in the Menderes Massif and covers an area of approximately 22 km2. In this part of the massif metamorphic complex comprises a sequence of different types of gneiss, metavolcanite and gamet micashists.
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Rudist bearing Upper Cretaceousmetamorphic sequences of the Menderes Massif (Western Turkey)
Geobios, 1998The Menderes Metamorphic Massif is located between the Izmir-Ankara zone to the north, and theLycianinappes and Bey Daglari platform to the south in the western part of Turkey. The massif consists of core rocks of Precambrian to Cambrian gneisses, schists, metagranites, and cover rocks of Paleozoic micaschists and marbles, Mesozoic thick bedded ...
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Les Zircons D'un Gneiss Oeillé du Menderes-Massif
1958Suivant les méthodes de Poldervaart (2, 3), l'auteur a fait l'étude deszircons provenant d'un gneiss oeillé du Menderes-massif d'origine controversée.Selon les uns les gneiss oeillés représenteraient d'ancienes granitesporphyroides. Sa texture alors serait blastoporphyrique.
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