Browsing by Author "Saraç G."
Now showing items 1-4 of 4
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Episodic graben formation and extensional neotectonic regime in west Central Anatolia and the Isparta Angle: A case study in the Aksehir-Afyon Graben, Turkey
Koçyi?it A.; Ünay E.; Saraç G. (2000)Central and Western Anatolia form a continental back-arc region related to the Hellenic-Cyprus convergent plate boundary of the Anatolian and African Plates. The Aksehir-Afyon Graben (AAG), the easternmost extension of the ... -
Halitpaşa transpressive zone: Implications for an early Pliocene compressional phase in Central Western Anatolia, Turkey
Kaya O.; Ünay E.; Saraç G.; Eichhorn S.; Hassenrück S.; Knappe A.; Pekde?er A.; Mayda S. (2004)The Late Cenozoic evolution of the eastern Aegean is dominated by widespread continental extension. The most prominent structures are E-W- and NE-SW-trending grabens and intervening horsts, while NW-SE- and N-S-trending ... -
Palynological analysis of neogene mammal sites of turkey - vegetational and climatic implications [Türkiye'de neojen memeli bulgu yerlerinden palinolojik analizler - vejetasyonel ve iklimsel çi{dotless}kari{dotless}mlar]
Yavuz Işik N.; Saraç G.; Ünay E.; de Bruijn H. (2011)Pollen assemblages from lacustrine sediments that have known positions relative to mammal faunas in central and western Turkey are analysed. The stratigraphical order of the pollen samples is based on the stage of evolution ... -
Tectonic implications of the Neogene stratigraphy of the Çankiri basin with special reference to the Çandir locality (North-Central Anatolia, Turkey)
Kaymakçi N.; De Bruijn H.; White S.H.; van Dijk P.M.; Saraç G.; Ünay E. (2003)The Çankiri Basin is straddled between the Sakarya continent of the Pontides in the north and the Kirşehir Block of Taurides. It includes Neogene units more than 1 km in thickness. Eight Neogene formations and two distinct ...