{"id":266,"date":"2017-11-16T15:44:21","date_gmt":"2017-11-16T13:44:21","guid":{"rendered":"http:\/\/blog.aku.edu.tr\/caglarozkaymak\/?page_id=266"},"modified":"2017-11-16T15:44:21","modified_gmt":"2017-11-16T13:44:21","slug":"tezler","status":"publish","type":"page","link":"https:\/\/blog.aku.edu.tr\/caglarozkaymak\/tezler\/","title":{"rendered":"Tezler"},"content":{"rendered":"

\t\t\t\t\u00a0Y\u00fcksek Lisans Tezi:<\/strong><\/p>\n

\u00d6zkaymak, \u00c7., 2003. Van \u015eehri ve Yak\u0131n \u00c7evresinin\u00a0Aktif Tektonik \u00d6zellikleri (Active Tectonic Properties of Van City and Nearby Area). Y\u00fcz\u00fcnc\u00fc Y\u0131l\u00a0\u00dcniversitesi, Fen Bilimleri Enstit\u00fcs\u00fc (Y\u00fcksek\u00a0Lisans Tezi), 76 s.<\/p>\n

\u00a0Doktora Tezi:<\/strong><\/p>\n

\u00d6zkaymak, \u00c7., 2012. Manisa Havzas\u0131’n\u0131n Aktif Tektoni\u011fi ve Depremselli\u011fi, Bat\u0131 Anadolu, T\u00fcrkiye (Active Tectonics and Seismicity of the Manisa Basin, western Anatolia, Turkey). Dokuz Eyl\u00fcl \u00dcniversitesi, Fen Bilimleri Enstit\u00fcs\u00fc (Doktora Tezi), 251 s.<\/p>\n

Y\u00fcksek Lisans Tezi \u00d6zet:\u00a0Van \u015eehri ve Yak\u0131n \u00c7evresinin\u00a0Aktif Tektonik \u00d6zellikleri<\/strong><\/p>\n

Bu \u00e7al\u0131\u015fma, Van \u015fehri yak\u0131n \u00e7evresinin aktif tektonik \u00f6zelliklerinin\u00a0belirlenmesi amac\u0131 ile, Y\u00fcz\u00fcnc\u00fc Y\u0131l \u00dcniversitesi, Fen Bilimleri Enstit\u00fcs\u00fc, Jeoloji\u00a0M\u00fchendisli\u011fi Anabilimdal\u0131 b\u00fcnyesinde Y\u00fcksek Lisans Tezi olarak haz\u0131rlanm\u0131\u015ft\u0131r.\u00a0Bu \u00e7al\u0131\u015fmada, Van \u015fehri yerle\u015fim alanlar\u0131 ve yak\u0131n \u00e7evresini kapsayan\u00a0b\u00f6lge \u00fczerine etkin aktif tektonizmaya i\u015faret eden bulgular sunulmu\u015ftur. Van G\u00f6l\u00fc\u00a0havzas\u0131 jeodinamik yap\u0131s\u0131n\u0131n tam olarak anla\u015f\u0131lmas\u0131na destek olacak bug\u00fcne kadar\u00a0haritalanmam\u0131\u015f yap\u0131sal unsurlar belirlenmeye \u00e7al\u0131\u015f\u0131lm\u0131\u015ft\u0131r. Bu yap\u0131lar\u0131n bilinen\u00a0mevcut yap\u0131sal unsurlar ile kontrol\u00fc ve ili\u015fkisi incelenmi\u015ftir. Bu kapsamda, Van\u00a0\u015fehri yerle\u015fim alanlar\u0131 ve yak\u0131n \u00e7evresi \u00fczerine etkin olabilecek aktif faylar\u0131n ve\u00a0gen\u00e7 tektonik yap\u0131lar\u0131n belirlenmesine \u00e7al\u0131\u015f\u0131lm\u0131\u015ft\u0131r. \u0130nceleme alan\u0131n\u0131n aktif\u00a0tektoni\u011fi; inceleme alan\u0131ndaki tektonik yap\u0131lar ile morfolojik yap\u0131lar\u0131n \u00f6zellikleri\u00a0incelenerek belirlenmi\u015ftir. \u0130nceleme alan\u0131n\u0131n morfolojik \u00f6zelliklerinin belirlenmesi\u00a0i\u00e7in topografik haritalardan faydalanarak \u00fcretilen, y\u00fcksek \u00e7\u00f6z\u00fcn\u00fcrl\u00fc\u011fe sahip say\u0131sal\u00a0arazi modeli \u00fczerinde \u00e7al\u0131\u015fmalar yap\u0131lm\u0131\u015ft\u0131r. Yap\u0131lan arazi \u00e7al\u0131\u015fmalar\u0131nda, b\u00f6lgedeki\u00a0aktif tektoni\u011fi karakterize eden faylar, \u00e7atlaklar, yelpazeler ve teraslar incelenmi\u015ftir.\u00a0T\u00fcm bunlarla birlikte, tarihsel ve aletsel d\u00f6neme ait verilerin kullan\u0131ld\u0131\u011f\u0131 bu\u00a0\u00e7al\u0131\u015fmada, depremlerin zaman i\u00e7erisindeki da\u011f\u0131l\u0131mlar\u0131 incelenmi\u015ftir. Son y\u0131llarda\u00a0Van G\u00f6l\u00fc i\u00e7ersinde ve \u00e7evresinde, k\u00fc\u00e7\u00fck ve orta \u015fiddetli deprem aktivitelerinin\u00a0say\u0131s\u0131nda yo\u011fun bir art\u0131\u015f g\u00f6zlenmektedir. Van \u015fehri kentsel yerle\u015fim alanlar\u0131na\u00a0yak\u0131n b\u00f6lgelerde 2000 \u2013 2002 y\u0131llar\u0131 aras\u0131nda meydana gelen orta \u015fiddetli\u00a0depremlerin odak \u00e7\u00f6z\u00fcmlemeleri de b\u00f6lgede kuzey-g\u00fcney s\u0131k\u0131\u015fmalar\u0131n\u0131n g\u00fcncel\u00a0varl\u0131\u011f\u0131n\u0131 g\u00f6stermektedir.\u00a0Sonu\u00e7 olarak, Van \u015eehri ve yak\u0131n \u00e7evresinin aktif tektonik \u00f6zelliklerinin ilk\u00a0olarak ayr\u0131nt\u0131l\u0131 bir \u015fekilde incelendi\u011fi bu \u00e7al\u0131\u015fmada inceleme alan\u0131ndaki Pliyo-Kuvaterner ve daha gen\u00e7 \u00e7\u00f6keller \u00fczerinde aktif tektonizmaya i\u015faret edebilecek\u00a0yap\u0131sal unsurlar belirlenmi\u015ftir. B\u00f6lge i\u00e7in \u00f6ng\u00f6r\u00fclen tektonik rejim modellemesi\u00a0yeni veri ve bulgular ile kar\u015f\u0131la\u015ft\u0131r\u0131lm\u0131\u015f, uygun olan destekleyici sonu\u00e7lara\u00a0ula\u015f\u0131lm\u0131\u015ft\u0131r. Elde edilen verilere g\u00f6re, bu b\u00f6lge, do\u011frultu at\u0131ml\u0131 faylar\u0131n bask\u0131n\u00a0oldu\u011fu Karl\u0131ova eklemi bat\u0131s\u0131 ile kar\u015f\u0131la\u015ft\u0131r\u0131ld\u0131\u011f\u0131nda \u00e7ok daha s\u0131k\u0131\u015fmal\u0131 bir tektonik\u00a0rejime sahiptir.<\/p>\n

MSc Thesis Abstract:\u00a0Active Tectonic Properties of Van City and Nearby Area<\/strong><\/p>\n

The aim of this study, prepared as a MSc thesis in Geological Engineering\u00a0program at Y\u00fcz\u00fcnc\u00fc Y\u0131l \u00dcniversity, is to determine the active tectonic properties of\u00a0the Van City and nearby areas. Main at the east of the largest lake of Turkey, the\u00a0Lake Van.\u00a0In this study, present some evidence showing active tectonics effected on\u00a0the region of Van city and nearby area. To understanding of the geodynamic\u00a0structure of the Lake Van Basin, some structural elements was unknown and some\u00a0them were determinated. The relation between new studied structures and known\u00a0structural elements is studied. Active faults and young structural elements are\u00a0investigated that evoluated arround Van city and will be effect strongly while getting\u00a0active. For this purpose, high resolution digital elevation models are prepared and\u00a0used in junction with satellite images to understand the morphologic characteristics\u00a0of the study area. Field observations undertaken in very recent fault zones reveal that\u00a0the area is under compression almost N-S, and extension, orientated E-S. This result\u00a0is in agrecment with the fault plane solutions obtained from three recent earthquakes\u00a0occurred near the southern shore of the Lake Van. Both historic and instrumental\u00a0seismic data used for identifying the seismotectonic characteristics of the study area.\u00a0The tectonic regime appears to be more compressional in this region when\u00a0compared to the west of the Karl\u0131ova junction where strike-slip faulting is thought to\u00a0dominate.<\/p>\n

Doktora Tezi \u00d6zet:\u00a0Manisa Havzas\u0131’n\u0131n Aktif Tektoni\u011fi ve Depremselli\u011fi, Bat\u0131 Anadolu, T\u00fcrkiye<\/strong><\/p>\n

\u00d6zet:\u00a0Gediz Grabeni’nin bat\u0131s\u0131nda yeralan Manisa Havzas\u0131, eski ve modern havza dolgu\u00a0birimleriyle birbirinden ayr\u0131lan iki evreli havza evrimine sahiptir. Eski havza dolgusu\u00a0birimleri k\u0131vr\u0131ml\u0131 ve fayl\u0131 Miyosen volkano-sedimanter istifinden olu\u015fur. Modern\u00a0havza dolgusu, karasal k\u0131r\u0131nt\u0131l\u0131 tortul kayalarla temsil edilen erken\u2013orta Pleyistosen\u00a0ya\u015fl\u0131 Turgutlu Formasyonu, akarsu \u00e7\u00f6kellerinden olu\u015fan Kuvaterner ya\u015fl\u0131 Bahad\u0131r\u00a0Alloformasyonu, ge\u00e7 Pleyistosen\u2013erken Holosen ya\u015fl\u0131 al\u00fcvyal\/kol\u00fcvyal \u00e7\u00f6kellerden\u00a0olu\u015fan Emlakdere Alloformasyonu ve al\u00fcvyal-fl\u00fcvyal \u00e7\u00f6kellerden olu\u015fan Manisa\u00a0Alloformasyonu ile temsil edilir. Yap\u0131sal ve stratigrafik veriler, havzan\u0131n ilk olarak\u00a0bat\u0131s\u0131ndan KD-GB uzan\u0131ml\u0131 volkanik s\u0131rt ile s\u0131n\u0131rl\u0131 bir g\u00f6l olarak olu\u015ftu\u011funu;\u00a0olas\u0131l\u0131kla Pliyosen’de etkili olan do\u011frultu at\u0131m bask\u0131n tektonizma ile aniden\u00a0y\u00fckselerek deformasyona u\u011frad\u0131\u011f\u0131n\u0131 g\u00f6stermektedir. \u0130zmir Bal\u0131kesir Transfer Zonu\u00a0(\u0130BTZ) boyunca etkili olan Miyosen sonras\u0131 do\u011frultu at\u0131ml\u0131 faylanma, Manisa\u00a0Havzas\u0131’nda sa\u011f y\u00f6nl\u00fc bir makaslama zonunun geli\u015fmesine neden olmu\u015ftur. Bu\u00a0durum, sa\u011f y\u00f6nl\u00fc Kuzey Anadolu Fay Zonu’nun baz\u0131 kollar\u0131n\u0131n Ge\u00e7 Pliyosen’de Bat\u0131\u00a0Anadolu Geni\u015fleme B\u00f6lgesi (BAGB) i\u00e7erisine do\u011fru hareket etti\u011fini g\u00f6stermektedir.\u00a0En gen\u00e7 Kuvaterner evre ise, KD-GB y\u00f6nl\u00fc geni\u015fleme bask\u0131n transtansiyon ile temsil\u00a0edilir. S\u00f6zkonusu tektonik ortamda olu\u015fan modern havza dolgusu bat\u0131dan KD-GB\u00a0uzan\u0131ml\u0131 do\u011frultu at\u0131ml\u0131, g\u00fcneyden ise D-B uzan\u0131ml\u0131 Manisa Fay Zonu (MFZ) ile\u00a0s\u0131n\u0131rl\u0131d\u0131r. MFZ, s\u0131ras\u0131yla 0,1, 0,3 ve 0,26 mm\/y\u0131l kayma h\u0131z\u0131na sahip bat\u0131, merkez ve\u00a0do\u011fu b\u00f6l\u00fcmler olmak \u00fczere \u00fc\u00e7 ana sismojenik zondan olu\u015fur. Bu \u00fc\u00e7 b\u00f6l\u00fcm boyunca\u00a0yap\u0131lan tektonik jeomorfoloji \u00e7al\u0131\u015fmalar\u0131 ve hesaplanan jeomorfolojik indisler, analiz\u00a0edilen fay segmentlerinin \u00e7izgisel gidi\u015fli ve y\u00fcksek derecede aktif oldu\u011funa i\u015faret\u00a0etmektedir.\u00a0MFZ’nun bat\u0131 b\u00f6l\u00fcm\u00fcnde ger\u00e7ekle\u015ftirilen paleosismoloji ama\u00e7l\u0131 hendek\u00a0\u00e7al\u0131\u015fmalar\u0131nda \u00fc\u00e7 depreme ait izler saptanm\u0131\u015ft\u0131r; bunlar s\u0131ras\u0131yla, 926, 1595 veya\u00a01664 ve 1845 depremlerine kar\u015f\u0131l\u0131k gelmektedir. Bu veriler, Manisa Havzas\u0131’ndaki\u00a0yerle\u015fim alanlar\u0131nda deprem tehlike analizlerine y\u00f6nelik \u00e7al\u0131\u015fmalar\u0131n \u00f6ncelikli olarak\u00a0yap\u0131lmas\u0131n\u0131 gerektirmektedir.<\/p>\n

Phd Thesis Abstract:\u00a0Active Tectonics and Seismicity of the Manisa Basin, western Anatolia, Turkey<\/strong><\/p>\n

The Manisa Basin, forming a connection with the Gediz Graben, has a two-stage\u00a0basin evolution, distinguished by an ancient and modern graben fill. The ancient\u00a0basin-fill is made up of a folded and normal-to-reverse faulted and strike-slip-faulted\u00a0Miocene volcano-sedimentary sequence. The younger modern basin-fill is\u00a0represented by the early-middle Pleistocene continental clastics of the Turgutlu\u00a0Formation, Quaternary Bahad\u0131r Alloformation comprising fluvial deposits,\u00a0alluvial\/colluvial sediments of late Pleistocene-early Holocene Emlakdere\u00a0Alloformation, and alluvial-fluvial sediments of Holocene Manisa Alloformation.\u00a0Structural and stratigraphical data reveal that the basin was initially formed as a\u00a0lacustrine basin bounded by a volcanic ridge from the west; it was subsequently\u00a0uplifted and deformed probably as a result of Pliocene wrench-dominated strike-slip\u00a0tectonics. Post-Miocene strike-slip faulting along the \u0130zmir Bal\u0131kesir Transfer Zone\u00a0(\u0130BTZ) occured along a right-lateral shear zone in the Manisa Basin. This suggests\u00a0that some branches of the right-lateral movement of the North Anatolia Fault\u00a0continues into the West Anatolian Extensional Province (WAEP). The youngest\u00a0stage shows an NE\u2012SW trending extension-dominated transtension. Modern graben\u00a0fill forming under the control of the youngest stage is bounded by NE-trending\u00a0strike-slip fault zone to the west and E\u2012W -trending Manisa Fault Zone (MFZ) to the\u00a0south. MFZ comprises three major seismogenic zones; western, central and eastern\u00a0sectors providing minimum slip rates of 0,1, 0,3 and 0,26 mm\/year, respectively.\u00a0Tectonic geomorphology studies and computed geomorphic indices along three\u00a0sectors suggest that the analyzed normal fault segments are linear and highly active.\u00a0On the western sector of the MFZ, we performed trenching studies and find evidence\u00a0for three palaeoearthquakes which correspond to 926 AD, 1595 or 1664 AD, with the\u00a0most recent event in 1845 AD. The results suggest that the earthquake risk\u00a0assessment for Manisa area is primarily essential.<\/p>\n","protected":false},"excerpt":{"rendered":"

\u00a0Y\u00fcksek Lisans Tezi: \u00d6zkaymak, \u00c7., 2003. Van \u015eehri ve Yak\u0131n \u00c7evresinin\u00a0Aktif Tektonik \u00d6zellikleri (Active Tectonic Properties of Van City and Nearby Area). Y\u00fcz\u00fcnc\u00fc Y\u0131l\u00a0\u00dcniversitesi, Fen Bilimleri Enstit\u00fcs\u00fc (Y\u00fcksek\u00a0Lisans Tezi), 76 s. \u00a0Doktora Tezi: \u00d6zkaymak, \u00c7., 2012. Manisa Havzas\u0131’n\u0131n Aktif Tektoni\u011fi ve Depremselli\u011fi, Bat\u0131 Anadolu, T\u00fcrkiye (Active Tectonics and Seismicity of the Manisa Basin, western Anatolia, … <\/p>\n

Devam\u0131n\u0131 oku<\/a><\/p>\n","protected":false},"author":7,"featured_media":0,"parent":0,"menu_order":0,"comment_status":"closed","ping_status":"closed","template":"","meta":{"footnotes":""},"class_list":["post-266","page","type-page","status-publish","hentry","nodate","item-wrap"],"_links":{"self":[{"href":"https:\/\/blog.aku.edu.tr\/caglarozkaymak\/wp-json\/wp\/v2\/pages\/266","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/blog.aku.edu.tr\/caglarozkaymak\/wp-json\/wp\/v2\/pages"}],"about":[{"href":"https:\/\/blog.aku.edu.tr\/caglarozkaymak\/wp-json\/wp\/v2\/types\/page"}],"author":[{"embeddable":true,"href":"https:\/\/blog.aku.edu.tr\/caglarozkaymak\/wp-json\/wp\/v2\/users\/7"}],"replies":[{"embeddable":true,"href":"https:\/\/blog.aku.edu.tr\/caglarozkaymak\/wp-json\/wp\/v2\/comments?post=266"}],"version-history":[{"count":0,"href":"https:\/\/blog.aku.edu.tr\/caglarozkaymak\/wp-json\/wp\/v2\/pages\/266\/revisions"}],"wp:attachment":[{"href":"https:\/\/blog.aku.edu.tr\/caglarozkaymak\/wp-json\/wp\/v2\/media?parent=266"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}