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Armutlu Peninsula
Late Cretaceous–Eocene Geological Evolution of the Pontides Based on New Stratigraphic and Palaeontologic Data Between the Black Sea Coast and Bursa (NW Turkey)
A New Classification of the Turkish Terranes and Sutures and Its Implication for the Paleotectonic History of the Region
Akinci Hepp Seismic Risk Assessment
The Generating Mechanisms of the August 17, 1999 I˙Zmit Bay (Turkey) Tsunami: Regional (Tectonic) and Local (Mass Instabilities) Causes
Middle-Late Eocene Marine Record of the Biga Peninsula, NW Anatolia, Turkey
Armutlu Yarımadası, Yalova) Morfotektoniğinin Jeomorfometrik Analizlerle Değerlendirilmesi
Neotectonics of the Southeast Marmara Region, NW Anatolia, Turkey
Megacity Istanbul Project Reports
Reply to Topical Editor Decision: Reconsider After Major Revisions
Seismic Parameters Re-Determined from Historical Seismograms Of
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Bulletin of the Mineral Research and Exploration
Active Faults and Evolving Strike-Slip Basins in the Marmara Sea, Northwest Turkey: a Multichannel Seismic Reflection Study
Population Change in Yalova Province
NORTH ANATOLIAN FAULT ZONE: Empirical Relations and the Changes
Uniform Basin Growth Over the Last 500Ka, North Anatolian Fault
Variations of Lithospheric Strength in Different Tectonic Settings
The Armutlu Network: an Investigation Into the Seismotectonic Setting of Armutlu–Yalova–Gemlik and the Surrounding Regions
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Continous Monitoring Microseismic Activity in the Eastern Marmara: the Armutlu Network
EGU2010-9961-1, 2010 EGU General Assembly 2010 © Author(S) 2010
Morphotectonic Development of the Marmara Region
The North Anatolian Fault on the Hersek Peninsula, Turkey: Its
How to Cite Complete Issue More Information About This Article
Yer-18-2-3-0803-4:Mizanpaj 1
Constraints on North Anatolian Fault Zone Width in the Crust and Upper Mantle from S-Wave Teleseismic Tomography
Guide Book Field Trip to the North Anatolian Fault System Between
Chap02.PDF 2 Geography, Geology and Hydrogeology of Marmara
Seismic Clustering in the Sea of Marmara Implications For
Crustal Density Model of the Sea of Marmara
THE NORTH ANATOLIAN FAULT: Anewlook
Multidisciplinary Analyses to Understand the Tectonic Activity and the Evolution
I RESOLVING the THROUGH-GOING ACTIVE FAULT GEOMETRY and FAULT STRENGTH PARAMETERS THROUGH STRESS MODELING: a STUDY of the NORTH ANATOLIAN FAULT (NAF)
Seven Years of Postseismic Deformation Following the 1999, M = 7.4 and M = 7.2, Izmit-Düzce, Turkey Earthquake Sequence
Earthquake Swarm in Armutlu Peninsula, Eastern Marmara Region, Turkey
How Far Did the Surface Rupture of the 1999 İzmit Earthquake
(2011): Geomechanical Model of the Marmara Sea Region - I