Cenzoic Anatolia

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Anatolian is a region in Turkey where vast amount of tectonic activity which was followed by magmatism took place during the Cenozoic era. The Anatolian microplate is bound to the north by the Mediterranean Sea, to the east by the Red sea and, to the south by the Aegean Sea. Ophiolites and suture zones seperate different pieces of continental blocks that came together to form the Anatolian microplate (Altunkaynak et al. 2012). Chorowicz (1999) defines Anatolia as a product of the African and Eurasian plate collision which formed mainly from lithospheric magma. A widespread of magmatism accompanied plate tectonism experienced in this region during the Cenozoic era. The late Eocene (37.3 ± 4.6, measure through K-Ar radiometric dating) marks the initial period where this magmatism in took place. This essay will establish if whether an East-west spatial control on the chemistry of Anatolian volcanics exists. Spatial control is a geographical process in space which didctates how the events of a certain process in space take place. East-west spatial control means that when moving from East-West are there geographical processes in space which are controlling the chemistry of Anatolian volcanics. The tectonic and magamatic activity that took place in Anatolia makes it a suitable place to study magma evolution as it preserves most of its volcanic rocks. Coban (2007) gave major subdivisions of the Anatolian microplate which are: the Eastern Anatolian collisional province (EACP), the central Anatolian province and, the Western Anatolian extensional province (WAEP) respectively. Two main tectonic processes are responsible for the distribution Anatolian volcanics and the process responsible are: the formation of topography related to the acc... ... middle of paper ... ... Reviews, 80(3), 219-238. Aldamaz, E., Pearce, J.A., Thirlwall, M.F., and Mitchell, J.G. (2000) Petrogenetic evolution of late Cenozoic, post-collision volcanism in western Anatolia, Turkey. Journal of Volcanology and Geothermal Research. 102(1-2). P.67-95. Seyítoǧlu, G., & Scott, B. C. (1996). The cause of NS extensional tectonics in western Turkey: tectonic escape vs back-arc spreading vs orogenic collapse. Journal of Geodynamics, 22(1), 145-153. SEN, P. A., TEMEL, A., & GOURGAUD, A. (2004). Petrogenetic modelling of Quaternary post-collisional volcanism: a case study of central and eastern Anatolia. Geological Magazine, 141(01), 81-98. Keskin, M. (2003). Magma generation by slab steepening and breakoff beneath a subduction-accretion complex: An alternative model for collision-related volcanism in Eastern Anatolia, Turkey. Geophysical Research Letters, 30(24), 8046

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