Yüksekokullar

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Citation - WoS: 147
Citation - Scopus: 157
The Geodynamics of the Aegean and Anatolia: Introduction
(2007) Taymaz, Tuncay; Yılmaz, Yücel; Dilek, Yıldırım R.; 01. Kadir Has University
[Abstract Not Available]
Citation - WoS: 20
Citation - Scopus: 25
Migration Asmovement Andmultiplace Life: Some Recent Developments in Rural Living Structures in Turkey
(Wiley-Blackwell, 2014) Öztürk, Murat; Hilton, Andy; Jongerden, Joost; 01. Kadir Has University
Discussing recent trends and developments in migration and mobility affecting what may be referred to as a reconstitution' of villages this paper discusses the changing character of rural settlement and settlement patterns in Turkey today. The binary division of rural and urban is questioned through a dialectical/relational approach to settlement formation while settlement is defined by relation to (human) movement itself understood as incorporating the modalities of migration and mobility. By focusing on the socio-economics of increasing affluence the advance of capital generally and the introduction of neoliberalism into agriculture in particular a number of contemporary rural-oriented (migratory/mobility) movements and living structures' are investigated which taken together suggest a growing development of dual settlement' and multiplace hybrid' life. The paper concludes with a typology of villages and some thoughts on the theoretical implications of this study. Copyright (c) 2013 John Wiley & Sons Ltd.
Citation - WoS: 38
Citation - Scopus: 46
Morphotectonic Development of the Marmara Region
(Elsevier Science Bv, 2010) Yılmaz, Yücel; Gokasan, Erkan; Erbay, A. Yücel; 01. Kadir Has University
The Marmara Region of northwest Turkey covers the Marmara Sea Basin and the surrounding lands. In the region morphologically different areas may be distinguished. The Marmara Sea Basin is a structural depression. The land to the north is known as the Thrace-Kocaeli Peneplain a flatland elevated above a horst. This may be referred to as the Istanbul Horst bounded by two strike-slip fault zones which define the structural boundaries of two sea basins

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