Muzaffer Özburan
Kocaeli University
10 Papers
166 Citations
Muzaffer Özburan is an academic researcher from Kocaeli University. The author has contributed to research in topics: North Anatolian Fault & Transpression. The author has an hindex of 6, co-authored 7 publications.
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Papers
Progressive development of the Büyük Menderes Graben based on new data, western Turkey
TL;DR: Oblique and normal fault systems exposed in the Buyuk Menderes Graben (BMG) region record two successive and independent complex tectonic events as discussed by the authors, which are responsible for the development of NW and NE-trending conjugate pairs of oblique faults which controlled Early Middle Miocene basin formation.
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Neotectonics of the SW Marmara region, NW Anatolia, Turkey
TL;DR: In this article, the geometrical and kinematic features of the faults in the region are described, based on field observations, and the Neogene and Quaternary basin fill which occupies large areas of the region has been determined, and tectonic regimes controlling these basins are explained.
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Complex basin evolution in the Gökova Gulf region: implications on the Late Cenozoic tectonics of southwest Turkey
Ömer Feyzi Gürer,Ercan Sangu,Muzaffer Özburan,Alper Gürbüz,Alper Gürbüz,Nuran Sarica-Filoreau +5 more
TL;DR: In this article, a transition from crustal shortening to extension during Late Cenozoic was recorded in four distinct basin types in the Mugla-Gokova Gulf region.
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Neotectonics of the southeast Marmara region, NW Anatolia, Turkey
TL;DR: In this article, the geometry and structural characteristics of the NAFZ in the southeast Marmara region and discusses the commencement age of the strike-slip tectonics using deformation patterns of Neogene units and information available in the literature.
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Late Cenozoic polyphase deformation and basin development, Kütahya region, western Turkey
TL;DR: The Kutahya region is of importance in the neotectonic evolution of western Anatolia because the strata contain clear evidence of compression and extension as discussed by the authors, and the region underwent erosion and lacustrine sediments accumulated in topographic lows between the late Miocene and the middle Pliocene.
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