2010
DOI: 10.1016/j.tecto.2009.05.012
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Morphotectonic development of the Marmara Region

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Cited by 45 publications
(35 citation statements)
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“…Previous studies dealing with the morphological development of the western part of the Marmara region (Yaltırak 1995;Elmas and Meriç 1998;Yaltırak et al 1998Yaltırak et al , 2000Gökaşan et al 2003;Yılmaz et al 2010), together with the recent seismic evidence, indicate that the morpho-tectonic evolution of the Çanakkale Basin may have started as the southern shelf area of the initial Marmara Sea under a N-S extensional regime at the end of the Late Miocene (Fig. 11a).…”
Section: Morpho-tectonic Evolution Of the çAnakkale Basinmentioning
confidence: 80%
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“…Previous studies dealing with the morphological development of the western part of the Marmara region (Yaltırak 1995;Elmas and Meriç 1998;Yaltırak et al 1998Yaltırak et al , 2000Gökaşan et al 2003;Yılmaz et al 2010), together with the recent seismic evidence, indicate that the morpho-tectonic evolution of the Çanakkale Basin may have started as the southern shelf area of the initial Marmara Sea under a N-S extensional regime at the end of the Late Miocene (Fig. 11a).…”
Section: Morpho-tectonic Evolution Of the çAnakkale Basinmentioning
confidence: 80%
“…The modern morphology of the Marmara region, which consists of the Marmara Sea and its surroundings, including the Biga and Gelibolu peninsulas, mostly reflects remnants of a mature horizontal erosion surface termed the ThraceKocaeli peneplain (Cvijic 1908;Pamir 1938;Emre et al 1998;Erinç 2000;Elmas 2003;Gökaşan et al 2005Gökaşan et al , 2008Yılmaz et al 2010). According to Yılmaz et al (2010), the erosion of this peneplain took place from the Late Oligocene to the end of the Late Miocene.…”
Section: Morpho-tectonic Situation In the Marmara Regionmentioning
confidence: 99%
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