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Dissertations / Theses on the topic 'Anatolian Plateau'

Author: Grafiati

Published: 4 June 2021

Last updated: 3 February 2022

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1

Radeff, Giuditta. "Geohistory of the Central Anatolian Plateau southern margin (southern Turkey)." Phd thesis, Universität Potsdam, 2014. http://opus.kobv.de/ubp/volltexte/2014/7186/.

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The Adana Basin of southern Turkey, situated at the SE margin of the Central Anatolian Plateau is ideally located to record Neogene topographic and tectonic changes in the easternmost Mediterranean realm. Using industry seismic reflection data we correlate 34 seismic profiles with corresponding exposed units in the Adana Basin. The time-depth conversion of the interpreted seismic profiles allows us to reconstruct the subsidence curve of the Adana Basin and to outline the occurrence of a major increase in both subsidence and sedimentation rates at 5.45 – 5.33 Ma, leading to the deposition of al

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2

Radeff, Giuditta [Verfasser], and Domenico [Akademischer Betreuer] Cosentino. "Geohistory of the Central Anatolian Plateau southern margin (southern Turkey) / Giuditta Radeff. Betreuer: Domenico Cosentino." Potsdam : Universitätsbibliothek der Universität Potsdam, 2014. http://d-nb.info/1058741004/34.

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3

Albino, Irene <1985&gt. "Thermochronological evolution of the Eastern Pontides and the Eastern Anatolian Plateau and NW Lesser Caucasus (Turkey, Georgia, Armenia)." Doctoral thesis, Alma Mater Studiorum - Università di Bologna, 2013. http://amsdottorato.unibo.it/5505/.

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The analysis of apatite fission tracks is applied to the study of the syn- and post-collisional thermochronological evolution of a vast area that includes the Eastern Pontides, their continuation in the Lesser Caucasus of Georgia (Adjara-Trialeti zone) and northern Armenia, and the eastern Anatolian Plateau. The resulting database is then integrated with the data presented by Okay et al. (2010) for the Bitlis Pütürge Massif, i.e. the western portion of the Bitlis-Zagros collision zone between Arabia and Eurasia. The mid-Miocene exhumation episode along the Black Sea coast and Lesser Caucasus o

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4

Biltekin, Demet. "Vegetation and climate of north anatolian and north aegean region since 7 Ma according to pollen analysis." Phd thesis, Université Claude Bernard - Lyon I, 2010. http://tel.archives-ouvertes.fr/tel-00720892.

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This study concerns a long marine section (DSDP Site 380: Late Miocene to Present) and onshore exposed sections from the Late Miocene and/or Early Pliocene. The main target of this study is to reconstruct vegetation and climate in the North Anatolia and North Aegean region for the last 7 Ma. Two vegetation types were alternately dominant: thermophilous forests and open vegetations including Artemisia steppes. During the Late Miocene, most of the tropical and subtropical plants declined because of the climatic deterioration. However, some of them survived during the Late Pliocene, such as those

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5

Dogan, Guray. "Comparison Of The Rural Atmosphere Aerosol Compositions At Different Parts Of Turkey." Master's thesis, METU, 2005. http://etd.lib.metu.edu.tr/upload/12605844/index.pdf.

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Long term data generated at four rural stations are compared to determine similarities and differences in aerosol compositions and factors contributing to observed differences at different regions in Turkey. The stations used in this study are located at Mediterranean coast (20 km to the west of Antalya city), Black Sea coast (20 km to the east of Amasra town), Central Anatolia (&Ccedil<br>ubuk, Ankara) and Northeastern part of the Anatolian Plateau (at Mt. Uludag). Data used in comparisons were generated in previous studies. However, some re-analysis of data were also performed<br>(1) to imp

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6

Tatar, Orhan. "Neotectonic structures in the east central part of the North Anatolian Fault Zone, Turkey." Thesis, Keele University, 1993. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.283263.

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7

Crespin, Anne-Sophie Pelon Olivier. "Le plateau anatolien de la fin de l'empire hittite aux invasions cimmeriennes, XIIe-VIIe siècle avant J.-C." [S.l.] : [s.n.], 2001. http://demeter.univ-lyon2.fr/sdx/theses/lyon2/2001/crespin_as.

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8

Crespin, Anne-Sophie. "Le plateau anatolien de la fin de l'empire hittite aux invasions cimmeriennes, XIIe-VIIe siècle avant J. -C." Lyon 2, 2001. http://theses.univ-lyon2.fr/documents/lyon2/2001/crespin_as.

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Pour aborder les problèmes de la transition entre l'âge du Bronze et celui du Fer et de l'apparition ensuite de nouvelles entités politiques sur le plateau anatolien, nous avons fait en premier lieu une présentation de la géographie de la région. Le second chapitre traite de l'historique des recherches sur le sujet avant et après la seconde guerre mondiale. Un sous chapitre est consacré à la présentation des dernières données. Les sources écrites classiques, égyptiennes, assyriennes, bibliques, cunéiformes et hiéroglyphiques et phrygiennes ont fourni des renseignements provenant de secteurs gé

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9

Biryol, Cemal Berk. "COMPLEX RUPTURE PROCESSES OF THE SOLOMON ISLANDS SUBDUCTION ZONE EARTHQUAKE AND SUBDUCTION CONTROLLED UPPER MANTLE STRUCTURE BENEATH ANATOLIA." Diss., The University of Arizona, 2009. http://hdl.handle.net/10150/194681.

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This dissertation explores subduction zone-related deformation both on short time scales in the form of subduction zone earthquakes and over larger time and geographical scales in the form of subduction rollback or detachment of the subducting lithosphere. The study presented here is composed of two parts. First, we analyzed the source-rupture processes of the April 1, 2007 Solomon Islands Earthquake (Mw=8.1) using a body-wave inversion technique. Our analysis indicated that the earthquake ruptured approximately 240 km of the southeast Pacific subduction zone in two sub-events.In the second pa

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10

Delph, Jonathan, and Jonathan Delph. "Crustal and Upper Mantle Structure of the Anatolian Plate: Imaging the Effects of Subduction Termination and Continental Collision with Seismic Techniques." Diss., The University of Arizona, 2016. http://hdl.handle.net/10150/622908.

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The neotectonic evolution of the eastern Mediterranean is intimately tied to interactions between the underthrusting/subducting slab along the southern margin of Anatolia and the overriding plate. The lateral variations in the subduction zone can be viewed as a temporal analogue of the transition between continuous subduction and subduction termination by continent-continent collision. By investigating the lateral variations along this subduction zone in the overriding plate, we can gain insight into the processes that precede continent collision. This dissertation summarizes the results of th

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11

Froger, Jean-Luc. "Apport des données géophysiques multi-sources pour l'identification des caldeiras du plateau de Nevsehir, Anatolie Centrale, Turquie. Classification texturale des formations volcaniques à partir de l'imagerie satellitaire." Clermont-Ferrand 2, 1996. http://www.theses.fr/1996CLF21789.

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Premiere partie: le champ volcanique de cappadoce est caracterise par une sequence de 10 ignimbrites neogenes. Les caldeiras associees ont ete en partie demantelees et enfouies sous l'effet des processus tectoniques et sedimentaires post-effondrement. Elles n'apparaissent donc plus dans le paysage actuel. De recents progres dans la comprehension de la stratigraphie et de la distribution des ignimbrites nous ont permis d'identifier deux zones sources principales pour les 6 plus importantes ignimbrites. Une etude detaillee de ces zones sources a ete menee sur la base de donnees gravimetriques, d

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12

Leeuw, Goverdina Anna Maria de. "The noble gas and carbon systematics of divergent, convergent and strike-slip plate boundaries examples from the Reykjanes Ridge, Central American Arc and North Anatolian Fault Zone /." Connect to a 24 p. preview or request complete full text in PDF format. Access restricted to UC campuses, 2007. http://wwwlib.umi.com/cr/ucsd/fullcit?p3259364.

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Thesis (Ph. D.)--University of California, San Diego, 2007.<br>Title from first page of PDF file (viewed June 22, 2007). Available via ProQuest Digital Dissertations. Vita. Includes bibliographical references (p. 190-209).

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13

Kementzetzidou, Despina. "Étude sismotectonique du sysème Thessalie-iles Sporades (Grèce centrale)." Grenoble 1, 1996. http://www.theses.fr/1996GRE10045.

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La deformation sismique dans la region de la thessalie, de l'eubee et des iles sporades est analysee a partir de donnees microsismiques. Ces donnees ont ete recueillies par un reseau sismologique de 70 stations, operationnel pendant une periode de 2 mois, qui a permis l'enregistrement de 434 seismes. La repartition de la sismicite marque les structures recentes de direction e-w en thessalie, mais aussi les failles de direction nw-se de l'eubee. L'alignement de sismicite observe sur la faille sud du golfe pagasitikos se prolonge vers les iles sporades selon une direction ene, en accord avec la

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14

Plummer, Charles Louis. "Searching for tectonic moments : geochemical tracers in young Anatolian basalts, Sivas, Turkey /." 2008. http://hdl.handle.net/10288/510.

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15

Chen, Chen-Tung, and 陳震東. "Exhumation History of the Lesser Caucasus and its Implication for Uplift of the Eastern Anatolia Plateau." Thesis, 2014. http://ndltd.ncl.edu.tw/handle/00212320172390366256.

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碩士<br>國立中正大學<br>應用地球物理研究所<br>102<br>The Lesser Caucasus, located on the Eastern Anatolia Plateau with 1500-2000 m high elevation, was resulted from the collision between the Arabian plate and Eurasia plate. Different models and initial timing have been proposed to infer the timing and mechanism of plateau building. Here we combined with U-Pb, zircon and apatite fission track dating of the Mesozoic to Eocene granite to reveal the exhumation history of the Lesser Caucasus. The U-Pb show it exist Mesozoic to Eocene granite intrusion in Lesser Caucasus. Most of the zircon fission track ages concen

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