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dc.contributor.authorKoral, H.
dc.contributor.authorHanilci, N.
dc.contributor.authorOzturk, Hüseyin
dc.date.accessioned2021-03-03T13:01:33Z
dc.date.available2021-03-03T13:01:33Z
dc.identifier.citationKoral H., Ozturk H., Hanilci N., "Tectonically induced coastal uplift mechanism of Gokceada Island, Northern Aegean Sea, Turkey", QUATERNARY INTERNATIONAL, cilt.197, ss.43-54, 2009
dc.identifier.issn1040-6182
dc.identifier.othervv_1032021
dc.identifier.otherav_317b9d2a-d88f-4ffb-95fc-c8a55efe4e33
dc.identifier.urihttp://hdl.handle.net/20.500.12627/37665
dc.identifier.urihttps://doi.org/10.1016/j.quaint.2008.04.001
dc.description.abstractThis paper presents evidence of coastal uplift on Gokceada (formerly Imbros) Island, situated in the northern Aegean Sea in proximity to it deep trough along the seismically active North Anatolian Fault (NAF). The island comprises 2 km thick sedimentary strata underlain by metamorphic rocks which are similar to those observed 170 km to the north in the Strandzha Rhodope Mountains. The sedimentary strata begin at the bottom with Eocene turbidites and limestones, continue upward with Oligocene-Lower Miocene detritial rocks and andesitic voicanoclastics, and end with loosely consolidated sandstones of the Upper Miocene Pliocene at the top. The island at its extreme eastern coast has a peneplain form. However, at its northern part it is mountainous and has steeply inclined coastal cliffs, uplifted paleo-shore notches, hanging valleys, springs, waterfalls, uncemented slope deposits, travertine formations, and exposed fault scarps. Field evidence of many coastal morphological, geological and tectonic features together with corresponding seismic reflection data suggest that the island has experienced it rapid uplift (i.e. vertical displacement) with respect to the Saros Trough along the NAF. Total uplift is on the order of a few kilometers since the initiation of the NAF during Pliocene (or late Pleistocene as suggested by some studies), and the yearly rate varies from a few millimeters to a centimeter according to the age assumed for this major fault. (c) 2008 Elsevier Ltd and INQUA. All rights reserved.
dc.language.isoeng
dc.subjectFiziki Coğrafya
dc.subjectJeoloji Mühendisliği
dc.subjectMühendislik ve Teknoloji
dc.subjectSosyal ve Beşeri Bilimler
dc.subjectCoğrafya
dc.subjectJEOLOJİ
dc.subjectYER BİLİMİ, MULTİDİSİPLİNER
dc.subjectTemel Bilimler (SCI)
dc.subjectYerbilimleri
dc.subjectCOĞRAFYA, FİZİKSEL
dc.titleTectonically induced coastal uplift mechanism of Gokceada Island, Northern Aegean Sea, Turkey
dc.typeMakale
dc.relation.journalQUATERNARY INTERNATIONAL
dc.contributor.departmentİstanbul Üniversitesi , ,
dc.identifier.volume197
dc.identifier.startpage43
dc.identifier.endpage54
dc.contributor.firstauthorID45596


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