The Gallipoli Caste ‹N the Byzantine Period
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Işgal Döneminde Izmir Metropoliti Hrisostomos (1919–1922)
Trakya Üniversitesi Sosyal Bilimler Dergisi 31 Haziran 2009 Cilt 11 Sayı 1 (31-50) İŞGAL DÖNEMİNDE İZMİR METROPOLİTİ HRİSOSTOMOS (1919–1922) Yrd. Doç. Dr. Bülent ATALAY* ÖZET Yunanistan, Mondros Mütarekesi’ne rağmen İzmir’i işgal etti. İşgalin gerçekleşmesinde İzmir Metropoliti Hrisostomos’un faaliyetleri çok etkili oldu. Hrisostomos, Türklerin, Hıristiyanları katlettiklerine dair iddialar ileri sürdü. Bunu ispat etmek için de "Türklerin Hıristiyanlara Tecavüzleri" adında bir kitap hazırlayarak işgalci devletlerin temsilciliklerine dağıttı. Metropolit Hirsostomos faaliyetlerini İzmir metropolithanesi merkezli yürütmekteydi. İşgalinin ilk gününde Yunan askerlerini karşılayan Hrisostomos, aynı zamanda onları kutsayarak, Türkleri öldürmenin görev olduğunu belirti. Ermenilerin de desteğini alan Metropolit Hrisostomos, İzmir’deki Türklere işgal süresince zor anlar yaşattı. Asıl amaç İzmir’in Yunanistan’a bağlanmasını sağlamaktı. İzmir Valisi İzzet’in de yardımı ile Hrisostomos Türkleri baskı altında tutmaya çalıştı. Fakat Yunan kuvvetlerinin, Türk ordusu karşısında almaya başladığı mağlubiyet, Hrisostomos’un ümitlerini kırmaya başladı. Türk kuvvetleri 9 Eylül 1922’de İzmir’e girdiler. Nihayet 10 Eylül 1922 tarihiyle birlikte Hrisostomos için yolun sonu da gelmişti. İzmir’de yaşayan Türkler tarafından linç edildi. Anahtar Kelime: Metropolit, Hrisostomos, İzmir, Millî Mücadele IZMIR ARCHBISHOP HRISOSTOMOS DURING THE INVASION (1919-1922) ABSTRACT Greece occupied lamis despite the Mondros Agreement. The activities of Izmir Archbishop Hrisostomos became effective on the invasion. Hrisostomos clamied that Turks murdered Christians. In order to prove this claim, he wrote o book named “Turks’ Attacks against Christions” and distributed it to the representations of the allied powers. Hrisostomos who welcomed the Grek troops and blessed them commanded the troops to kill Turks. Hrisostomos who was supported by the Armanions caused to hard times for Turks during the invasion. -
Seismic Reflection, Well Log, and Gravity Analysis of the Thrace
BearWorks MSU Graduate Theses Spring 2016 Seismic Reflection, ellW Log, And Gravity Analysis Of The Thrace Basin, Northwestern Turkey Murat Kuvanc As with any intellectual project, the content and views expressed in this thesis may be considered objectionable by some readers. However, this student-scholar’s work has been judged to have academic value by the student’s thesis committee members trained in the discipline. The content and views expressed in this thesis are those of the student-scholar and are not endorsed by Missouri State University, its Graduate College, or its employees. Follow this and additional works at: https://bearworks.missouristate.edu/theses Part of the Geology Commons, and the Geophysics and Seismology Commons Recommended Citation Kuvanc, Murat, "Seismic Reflection, ellW Log, And Gravity Analysis Of The Thrace Basin, Northwestern Turkey" (2016). MSU Graduate Theses. 2372. https://bearworks.missouristate.edu/theses/2372 This article or document was made available through BearWorks, the institutional repository of Missouri State University. The work contained in it may be protected by copyright and require permission of the copyright holder for reuse or redistribution. For more information, please contact [email protected]. SEISMIC REFLECTION, WELL LOG, AND GRAVITY ANALYSIS OF THE THRACE BASIN, NORTHWESTERN TURKEY A Master Thesis Presented to The Graduate College of Missouri State University In Partial Fulfillment Of the Requirements for the Degree Master of Natural Applied Sciences By Murat Kuvanc May, 2016 Copyright 2016 by Murat Kuvanc ii SEISMIC REFLECTION, WELL LOG, AND GRAVITY ANALYSIS OF THE THRACE BASIN, NORTHWESTERN TURKEY Geography, Geology, and Planning Missouri State University, May 2016 Master of Natural Applied Sciences Murat Kuvanc ABSTRACT The Thrace basin is located between the Paleogene the Istranca and Rhdope massifs in the northwestern part of Turkey. -
Geology and Geochronology of Mineral Deposits in the Biga Peninsula, NW Turkey
OREGEO-00920; No of Pages 31 Ore Geology Reviews xxx (2012) xxx–xxx Contents lists available at SciVerse ScienceDirect Ore Geology Reviews journal homepage: www.elsevier.com/locate/oregeorev A prospective sector in the Tethyan Metallogenic Belt: Geology and geochronology of mineral deposits in the Biga Peninsula, NW Turkey Ozcan Yigit ⁎ Department of Geological Engineering, Canakkale Onsekiz Mart University, Canakkale 17020, Turkey article info abstract Article history: The Tethyan Metallogenic Belt (TMB), extending from Europe through Anatolia to Iran, is one of the world's major Received 18 December 2010 metal producing belts, and consists of many sectors. Mineral deposits of the Biga Peninsula in northwestern Received in revised form 2 June 2011 Turkey exhibit, in many ways, the characteristics of mineral deposits found throughout the belt. Biga Peninsula Accepted 29 September 2011 tectonically forms the westernmost part of the Sakarya Zone and easternmost part of the Rhodope Zone at the Available online xxxx intersection of Gondwana and Laurasia. The Biga Peninsula metallogeny research and exploration project created a GIS inventory of mineral deposits Keywords: fi Turkey and prospects, and classi ed them genetically to evaluate the mineral deposit potential using genetic models Biga Peninsula based on descriptive data. The GIS database, consisting of 128 deposits or prospects, helped to generate new Geochronology prospects and potential prospects. This field-based study indicated that the Biga Peninsula forms a prime tar- Tethyan metallogeny get for gold–copper exploration not only in Turkey but in the world. Porphyry Au–Cu–Mo The current economically significant mineral deposits of the Biga Peninsula were shaped by Cenozoic calc- Epithermal alkaline magmatism, ranging between 52 and 18 Ma, and related to mainly collisional and post-collisional Skarn tectonic regime. -
AYDINOĞLU ĠBRAHĠM BEY VE BODAMYA MESELESĠ AYDINOGLU IBRAHIM BEY and BODAMIA ISSUE Funda ADITATAR
TAD, C.39/S.68, 2020, s.175-205 AYDINOĞLU ĠBRAHĠM BEY VE BODAMYA MESELESĠ AYDINOGLU IBRAHIM BEY AND BODAMIA ISSUE Funda ADITATAR Makale Bilgisi Article Info Başvuru: 10.06.2020 Received: June 10, 2020 Kabul: 10.09.2020 Accepted: September 10, 2020 Özet Aydınoğlu Beyliği, on dördüncü yüzyıl başlarında Batı Anadolu’da kurulmuş Türk beyliklerinden biridir. Kurucusu Aydınoğlu Mehmet Bey, Birgi, Tire, Efes/Ayasuluk, Yukarı İzmir Kalesini topraklarına kattı. Merkezi Birgi olan beylik hakkında bilgi edinilen başlıca kaynak, on beşinci yüzyılda yazılmış olan Düstürnâme-i Enverî adlı eserdir. Buna göre Mehmet Bey hâkimiyeti altındaki yerleri, beş oğlu arasında paylaştırarak her birini idareci olarak kendi bölgesine tayin etmiştir. Ayasuluğ ve Sultanhisarı'nı büyük oğlu Hızır Bey'e, İzmir'i Umur Bey'e, Bodamya'yı üçüncü oğlu İbrahim Bahadır Bey'e, Tire'yi dördüncü oğlu Süleyman Bey'e vermiştir. En küçük oğlu İsa Bey'i de yanında alıkoymuştur. İbrahim Bahadır Bey’e verilen Bodamya’nın, günümüzde İzmir Ödemiş’te Bademli olduğu genel kabul görmüştür. Ancak bu iddia, Mehmet Bey’in ikametgahı Birgi ile Süleyman’ın bölgesi Tire’ye yakınlığından dolayı sorunludur. Urla’nın sosyal ve iktisadi tarihine ilişkin yapılan çalışmada bölgenin, Aydınoğlu Beyliği hakimiyetine girişiyle uzun soluklu bir dönüşüm geçirdiği anlaşılmıştır. Bu dönüşümü anlama gayreti, Bodamya’nın yeri ile ilgili yeni bir tespitin de mümkün olabileceğini ortaya çıkarmıştır. Bu tespite; dönemin iktisadi ve siyasi olaylarıyla İbrahim Bey’in fetih ve idari faaliyetlerinin yeniden değerlendirilmesiyle ulaşılmıştır. Dolayısıyla bu makale, Urla Yarımadası’nın tarihi gelişimi yanında Aydınoğlu Beyliği’nin idari yapısına, tarihi bir figür olarak İbrahim Bey’in tanınmasına katkı sağlamayı amaçlamaktadır. Anahtar Kelimeler: Aydınoğlu Beyliği, İbrahim Bey, Bodamya, Urla, Tarihi Coğrafya Abstract Aydinoglu emirate is founded in Western Anatolia in the beginning of the fourteenth century. -
Tc. Süleyman Demirel Üniversitesi Sosyal Bilmler Enstitüsü Tarih Anabilim Dali
TC. SÜLEYMAN DEMİREL ÜNİVERSİTESİ SOSYAL BİLMLER ENSTİTÜSÜ TARİH ANABİLİM DALI ORTAÇAĞ ANADOLU’SUNDA İSTANBUL İLE AFYONKARAHİSAR ARASINDAKİ ASKERİ YOL GÜZERGÂHLARI Seda EDİZ 1130204513 YÜKSEK LİSANS TEZİ DANIŞMAN Doç. Dr. Abdullah BAKIR ISPARTA-2019 (Ediz, Seda, Ortaçağ Anadolu’sunda İstanbul ile Afyonkarahisar Arasındaki Askeri Yol Güzergâhları, Yüksek Lisans Tezi, Isparta, 2018) ÖZET Yapılan bu tez çalışmasında İstanbul-Afyonkarahisar arasındaki askeri yol güzergahları ve bu iki şehir arasında kalan bölgenin tarihi coğrafyası hakkında bilgiler verilmektedir. Bu bağlamda öncelikle Eski Çağda bölgenin tarihi coğrafyası ve bu dönemde gerçekleşmiş, söz konusu saha üzerinden yapılan veya bu yollardan geçen savaşlar ele alınmıştır. Ardından Orta Çağda gerçekleşen Bizans Selçuklu mücadeleleri sırasında kullanılan yol güzergahları değerlendirilmiş sonrasında ise I., II., ve III. Haçlı Seferleri esnasında kullanılan yol güzergahları ana kaynaklar ve topografik eserler yardımı ile incelenmeye alınmıştır. Çalışmada konunun aydınlatılmasına yardımcı olması açısından söz konusu sahanın tarihi coğrafyası, Bithynia, Mysia, Troas, Aiolis, Lydia, Ionia ve Phrygia olacak şekilde sırasıyla ele alınmıştır. Tarihi coğrafya incelendikten sonra Eski Çağda bölgeden geçen askeri yol güzergahını kullanmış orduların savaşlarına kronolojik olarak yer verilmiştir. Öncelikle Pers kral yolu değerlendirilmiş ardından, Pers Kralı Kserkses’in Yunanistan Seferi (MÖ. 481-480) sırasında Anadolu’da izlediği yol güzergahı ve savaş esnasında yaşanan olaylara yer verilmiştir. -
Change and Continuity in the Sivas Province, 1908
CHANGE AND CONTINUITY IN THE S İVAS PROVINCE, 1908-1918 A THESIS SUBMITTED TO THE GRADUATE SCHOOL OF SOCIAL SCIENCES OF MIDDLE EAST TECHNICAL UNIVERSITY BY DEN İZ DÖLEK IN PARTIAL FULFILLMENT OF THE REQUIREMENTS FOR THE DEGREE OF MASTER OF ARTS IN THE DEPARTMENT OF HISTORY SEPTEMBER 2007 Approval of the Graduate School of Social Sciences Prof. Dr. Sencer Ayata Director I certify that this thesis satisfies all the requirements as a thesis for the degree of Master of Arts Prof. Dr. Seçil Karal Akgün Head of Department This is to certify that we have read this thesis and that in our opinion it is fully adequate, in scope and quality, as a thesis for the degree of Master of Arts. Assist. Prof. Dr. Nesim Şeker Supervisor Examining Committee Members Assoc. Prof. Dr. Bilge Nur Criss (Bilkent, IR) Assist. Prof. Dr. Nesim Şeker (METU, HIST) Assoc. Prof. Dr. Recep Boztemur (METU, HIST) I hereby declare that all information in this document has been obtained and presented in accordance with academic rules and ethical conduct. I also declare that, as required by these rules and conduct, I have fully cited and referenced all material and results that are not original to this work. Name, Last name : Deniz Dölek Signature : iii ABSTRACT CHANGE AND CONTINUITY IN THE S İVAS PROVINCE, 1908-1918 Dölek, Deniz M. A., Department of History Supervisor: Assist. Prof. Dr. Nesim Şeker September 2007, 146 pages Second Constitutional Era (1908-1918) was a period within which great changes occurred in the Ottoman Empire. On the one hand, it was a part of the modernization process that began in late eighteenth century; on the other hand, it was the last period of the Empire that had its own dynamics. -
A New Classification of the Turkish Terranes and Sutures and Its Implication for the Paleotectonic History of the Region
Available online at www.sciencedirect.com Tectonophysics 451 (2008) 7–39 www.elsevier.com/locate/tecto A new classification of the Turkish terranes and sutures and its implication for the paleotectonic history of the region ⁎ Patrice Moix a, , Laurent Beccaletto b, Heinz W. Kozur c, Cyril Hochard a, François Rosselet d, Gérard M. Stampfli a a Institut de Géologie et de Paléontologie, Université de Lausanne, CH-1015 Lausanne, Switzerland b BRGM, Service GEOlogie / Géologie des Bassins Sédimentaires, 3 Av. Cl. Guillemin - BP 36009, FR-45060 Orléans Cedex 2, France c Rézsü u. 83, H-1029 Budapest, Hungary d IHS Energy, 24, chemin de la Mairie, CH-1258 Perly, Switzerland Received 15 October 2007; accepted 6 November 2007 Available online 14 December 2007 Abstract The Turkish part of the Tethyan realm is represented by a series of terranes juxtaposed through Alpine convergent movements and separated by complex suture zones. Different terranes can be defined and characterized by their dominant geological background. The Pontides domain represents a segment of the former active margin of Eurasia, where back-arc basins opened in the Triassic and separated the Sakarya terrane from neighbouring regions. Sakarya was re-accreted to Laurasia through the Balkanic mid-Cretaceous orogenic event that also affected the Rhodope and Strandja zones. The whole region from the Balkans to the Caucasus was then affected by a reversal of subduction and creation of a Late Cretaceous arc before collision with the Anatolian domain in the Eocene. If the Anatolian terrane underwent an evolution similar to Sakarya during the Late Paleozoic and Early Triassic times, both terranes had a diverging history during and after the Eo-Cimmerian collision. -
Freshwater Fish Fauna and Restock Fish Activities of Reservoir in the Dardanelles (Canakkale-Turkey)
Journal of Central European Agriculture, 2012, 13(2), p.368-379 DOI: 10.5513/JCEA01/13.2.1062 Freshwater fish Fauna and Restock Fish Activities of Reservoir in the Dardanelles (Canakkale-Turkey) Selcuk BERBER1, Hüseyin SASI 2 1Department of Freshwater Biology, Fisheries Faculty, C. Onsekizmart University, Canakkale, Turkiye e-mail: [email protected] 2Department of Freshwater Biology, Fisheries Faculty, Mugla University, 48100, Mugla, Turkiye e-mail: [email protected] Abstract Turkey has, with geographic location including Istanbul and Çanakkale straits the system, 178,000 km in length streams, 906,000 ha of natural lakes, and 411,800 ha of dam lakes, and 28,000 ha of ponds due to richness inland waters which include freshwater fish. The fingerling fish (fry) were restocked approximately 250,000,000 in natural lakes, dam lakes and ponds for fisheries between years of 1979 and 2005. Canakkale has rich freshwater potential with 7 major rivers (Büyükdere, Karamenderes stream, Kavak brook, Kocacay stream, Sarıcay stream, Tuzla brook, Umurbey brook), 7 Dam Lakes (Atikhisar, Zeytinlikoy, Bayramic, Bakacak, Tayfur, Umurbey and Yenice-Gönen Dam lakes). In the studies, it has been determined that 15 fish species belonging to 6 families (Anguillidae, Atherinidae, Salmonidae, Cobitidae, Cyprinidae and Poecilidae) can be found in reservoirs. Fish restocking of the activities of the reservoir until today approximately 1,120,000 (Cyprinus carpio L., 1758) is introduced. In this study, the activity of Canakkale province in the fish restocking and reservoir exploiting possibilities were discussed in view of reservoir fisheries potential which is used insufficiently today. Keywords: Fish fauna, Dardanelles, Freshwater fish, Canakkale, Restocking Introduction Addition to being surrounded by Black Sea, Aegean Sea and Mediterranean Sea Turkey has a great freshwater potential with 178,000 km long streams and 906,000 ha natural lakes, 439,800 ha dam lakes and pond areas. -
Turkish Studies International Periodical for the Languages, Literature and History of Turkish Or Turkic Volume 11/1 Winter 2016, P
Turkish Studies International Periodical for the Languages, Literature and History of Turkish or Turkic Volume 11/1 Winter 2016, p. 59-76 DOI Number: http://dx.doi.org/10.7827/TurkishStudies.9157 ISSN: 1308-2140, ANKARA-TURKEY Article Info/Makale Bilgisi Received/Geliş: 19.01.2016 Accepted/Kabul: 08.03.2016 Referees/Hakemler: Prof. Dr. Ayşe ÇAYLAK TÜRKER – Doç. Dr. Ferudun ÖZGÜMÜŞ This article was checked by iThenticate. DARKALE IN THE BYZANTINE PERIOD: SETTLEMENT AND SOME ARCHITECTURAL NOTES Ü. Melda ERMİŞ* ABSTRACT Darkale, which was included in the Mysia region in Antiquity, was within the territorium of Pergamon, an important city of the Roman Empire after the Kingdom of Pergamon. When the Roman Empire was divided into two parts, the area became a part of the Eastern Roman Empire. The plains irrigated by River Kaikos (Bakırçay) enriched the region while Tırhala Mountain remained as fortified defence. Owing to its advantageous location, Darkale must have been an important settlement during the Byzantine Period as well. This settlement was especially included in the theme of Neokastra in order to stop Turkish raids into Western Anatolia, and also to reinforce regional defense and protect the settlements. There are various opinions on the Byzantine Period settlement in Darkale. Germe, Thrakoula and Khliara are possibilities on which the researchers dwell. Although we do not possess the epigraphic data necessary to positively define the settlement in Darkale, etymological change of its name, historical development and architectural remains of a defence system in the area from the Byzantine Period support the possibility of Khliara. STRUCTURED ABSTRACT The exact date of settlement in Darkale, which is currently a village within the town of Soma in the city of Manisa, is not clear; however, there are varied opinions on its presence and name during the Byzantine Period. -
Middle-Late Eocene Marine Record of the Biga Peninsula, NW Anatolia, Turkey
Geologica Acta, Vol.16, Nº 2, June 2018, 163-187, I DOI: 10.1344/GeologicaActa2018.16.2.4 E. Özcan, A.I. Okay, K.A. Bürkan, A.O. Yücel, Z. Özcan, 2018 CC BY-SA Middle-Late Eocene marine record of the Biga Peninsula, NW Anatolia, Turkey E. ÖZCAN1 A.I. OKAY1, 2 K.A. BÜRKAN3 A.O. YÜCEL1 Z. ÖZCAN2 1İstanbul Technical University, Faculty of Mines, Department of Geological Engineering Maslak 34469, İstanbul, Turkey. Özcan E-mail: [email protected], [email protected] 2İstanbul Technical University, Eurasia Institute of Earth Sciences Maslak 34469, İstanbul, Turkey 3Turkish Petroleum Corporation Mustafa Kemal Mah. 2. Cad., No. 86, 06520 Söğütözü, Ankara, Turkey ABS TRACT The Eocene shallow marine deposits marking the first marine incursion in the Biga Peninsula (NW Turkey) after the collision of the Sakarya and Anatolide-Tauride plates were investigated based on paleontological, litho- and chrono-stratigraphic data. Larger Benthic Foraminifera (LBF) from patchily distributed outcrops were studied in order to i) revise the stratigraphy of Eocene shallow marine units, and ii) establish a modern biostratigraphic setting and a correlation scheme. The Şevketiye Formation (Fm.) is herein defined as a predominantly shallow marine clastic deposit with subordinate carbonates overlying the Çamlıca metamorphic rocks, and passing laterally to the Soğucak Fm., a carbonate unit that is widely represented in the Thrace Basin. The record of alveolinids, primitive developmental stages of heterosteginids, and orthophragminids in the Şevketiye Fm. suggests that this formation is part of the Shallow Benthic Zones (SBZ) 16?/17 (Late Lutetian?/Early Bartonian), SBZ17?/18 and SBZ19A (Early Bartonian/earliest Priabonian). -
CHG Library Book List
CHG Library Book List (Belgium), M. r. d. a. e. d. h. (1967). Galerie de l'Asie antérieure et de l'Iran anciens [des] Musées royaux d'art et d'histoire, Bruxelles, Musées royaux d'art et dʹhistoire, Parc du Cinquantenaire, 1967. Galerie de l'Asie antérieure et de l'Iran anciens [des] Musées royaux d'art et d'histoire by Musées royaux d'art et d'histoire (Belgium) (1967) (Director), T. P. F. H. (1968). The Metropolitan Museum of Art Bulletin: Volume XXVI, Number 5. New York: Metropolitan Museum of Art (January, 1968). The Metropolitan Museum of Art Bulletin: Volume XXVI, Number 5 by Thomas P.F. Hoving (1968) (Director), T. P. F. H. (1973). The Metropolitan Museum of Art Bulletin: Volume XXXI, Number 3. New York: Metropolitan Museum of Art (Ed.), A. B. S. (2002). Persephone. U.S.A/ Cambridge, President and Fellows of Harvard College Puritan Press, Inc. (Ed.), A. D. (2005). From Byzantium to Modern Greece: Hellenic Art in Adversity, 1453-1830. /Benaki Museum. Athens, Alexander S. Onassis Public Benefit Foundation. (Ed.), B. B. R. (2000). Christian VIII: The National Museum: Antiquities, Coins, Medals. Copenhagen, The National Museum of Denmark. (Ed.), J. I. (1999). Interviews with Ali Pacha of Joanina; in the autumn of 1812; with some particulars of Epirus, and the Albanians of the present day (Peter Oluf Brondsted). Athens, The Danish Institute at Athens. (Ed.), K. D. (1988). Antalya Museum. İstanbul, T.C. Kültür ve Turizm Bakanlığı Döner Sermaye İşletmeleri Merkez Müdürlüğü/ Ankara. (ed.), M. N. B. (Ocak- Nisan 2010). "Arkeoloji ve sanat. (Journal of Archaeology and Art): Ölümünün 100.Yıldönümünde Osman Hamdi Bey ve Kazıları." Arkeoloji Ve Sanat 133. -
Neotectonics of the Southeast Marmara Region, NW Anatolia, Turkey
Journal of Asian Earth Sciences 21 (2003) 1041–1051 www.elsevier.com/locate/jseaes Neotectonics of the southeast Marmara region, NW Anatolia, Turkey O¨ mer Feyzi Gu¨rer*, Nuretdin Kaymakc¸ı, S¸erafeddin C¸ akır, Muzaffer O¨ zburan Kocaeli University, Engineering Faculty, Department of Geology, Kocaeli TR 41100, Turkey Received 26 October 2001; revised 24 May 2002; accepted 4 September 2002 Abstract The North Anatolian Fault Zone (NAFZ) bifurcates into three branches in the Marmara Region, which is a transition zone between the strike–slip tectonics manifested by the NAFZ and the N–S directed extensional regime of western Anatolia. The southern Marmara region is characterized by the middle and the southern branches while the northern branch controls the north Marmara region. The south Marmara region is characterized by approximately E–W trending rhomb-like horst and graben complexes bounded by strike slip-faults with normal component, striking mainly in E–W direction. This study documents the geometry and the 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. q 2002 Elsevier Science Ltd. All rights reserved. Keywords: Marmara sea; Neotectonics; North Anatolian fault zone; Extensional regime 1. Introduction regime which causes N–S extension of western Anatolia and the Aegean Sea area and (2) the strike–slip tectonics exerted Turkey has suffered two severe earthquakes that occurred by the NAFZ. The former is effective in a broad zone from along two segments of the North Anatolian Fault Zone Bulgaria in the north to the Hellenic trench in the south (NAFZ) on 17 August 1999 (Mw 7.4) and 12 November (McKenzie, 1972).