2013
DOI: 10.1016/j.jog.2012.06.009
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Structural evidence for strike-slip deformation in the İzmir–Balıkesir transfer zone and consequences for late Cenozoic evolution of western Anatolia (Turkey)

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Cited by 83 publications
(57 citation statements)
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“…In this sense, understanding the spatial and temporal relationships between E-W and NE-SW trending structures within the context of inception and evolution of large-scale fault systems play an important role in understanding the complex deformational history of the region (Bozkurt & Sözbilir, 2006;Çiftçi & Bozkurt, 2007;Gürboğa, 2014). Koçyiğit & Özaçar, 2003;Kaymakci et al, 2007;Uzel et al, 2013). (b) Simplified tectonic map of western Anatolia (after Sözbilir et al, 2011).…”
Section: Geological Settingmentioning
confidence: 99%
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“…In this sense, understanding the spatial and temporal relationships between E-W and NE-SW trending structures within the context of inception and evolution of large-scale fault systems play an important role in understanding the complex deformational history of the region (Bozkurt & Sözbilir, 2006;Çiftçi & Bozkurt, 2007;Gürboğa, 2014). Koçyiğit & Özaçar, 2003;Kaymakci et al, 2007;Uzel et al, 2013). (b) Simplified tectonic map of western Anatolia (after Sözbilir et al, 2011).…”
Section: Geological Settingmentioning
confidence: 99%
“…Since then, a considerable amount of new information has been accumulated (Bozkurt, 2003;Bozkurt & Sözbilir, 2006;Kaymakci, 2006;Koçyiğit et al, 1999;Özkaymak et al, 2013;Sözbilir et al, 2008Sözbilir et al, , 2011Sümer, 2015;Sümer et al, 2013;Uzel, Sözbilir, & Özkaymak, 2012;Uzel et al, 2013). Most of these studies are related to the development and evolution of the İBTZ.…”
Section: Evolution and Bearings Of Kfz Within The West Anatolian Tectmentioning
confidence: 99%
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“…The interruption of ductile exhumation in Middle Miocene, in all types of metamorphic rocks (HT as well as HP) whatever their age of onset, as well as the segmentation of the metamorphic units and the deposition of Neogene basins on top of them suggest that the transition between the two modes of extension was not progressive and likely occurred in a rather short delay. The Myrthes-Ikaria fault (MIF) (Philippon et al, 2012) that cut trough the whole Cyclades domain is the offshore extend of the onshore Ismir-Balikeshir transfer zone (IBTZ) (Sozbilir et al, 2010;Ersoy et al, 2012;Uzel et al, 2013) (Fig. 4).…”
Section: Stage 2: Neogene Basins and Dextral Transtensional Faultingmentioning
confidence: 99%