Balanced Cross Section of the Northeast of Adiyaman, Turkey

Total Page:16

File Type:pdf, Size:1020Kb

Balanced Cross Section of the Northeast of Adiyaman, Turkey Scholars' Mine Masters Theses Student Theses and Dissertations 2013 Balanced cross section of the northeast of Adiyaman, Turkey Mustafa Tuncer Follow this and additional works at: https://scholarsmine.mst.edu/masters_theses Part of the Geology Commons, and the Geophysics and Seismology Commons Department: Recommended Citation Tuncer, Mustafa, "Balanced cross section of the northeast of Adiyaman, Turkey" (2013). Masters Theses. 7580. https://scholarsmine.mst.edu/masters_theses/7580 This thesis is brought to you by Scholars' Mine, a service of the Missouri S&T Library and Learning Resources. This work is protected by U. S. Copyright Law. Unauthorized use including reproduction for redistribution requires the permission of the copyright holder. For more information, please contact [email protected]. BALANCED CROSS SECTION OF THE NORTHEAST OF ADIYAMAN, TURKEY by MUSTAFA TUNCER A THESIS Presented to the Faculty of the Graduate School of the MISSOURI UNIVERSITY OF SCIENCE AND TECHNOLOGY In Partial Fulfillment of the Requirements for the Degree MASTER OF SCIENCE IN GEOLOGY&GEOPHYSICS 2013 Approved by John Patrick Hogan, Advisor Kelly Liu Stephen Gao 2013 MUSTAFA TUNCER All Rights Reserved iii ABSTRACT Deformation during closure of an ocean basin and continent-continent collision in southeast Anatolia Turkey during the Late Cretaceous to Middle Miocene was investigated by construction of a geologic map, structural cross-section and retrodeformed palinspastically restored cross-section. The area of study is a N-S transect across the Bitlis Suture Zone of Northeast of Adiyaman. The study area is situated in the southeast Anatolian orogenic belt which includes, from south to north, the Arabian platform, the zone of Imbrication, and the zone of Nappes. A geologic map of this region was prepared in order to construct balanced and restored cross sections from the Bitlis Suture Zone, Northeast of Adiyaman, Turkey. This balanced cross section integrates surface and subsurface data to analyze the structural geometry of the region, calculate the vertical extension and tectonic shortening. The cross section was restored using the line and area balancing methods. A balanced structural cross section suggests that structural uplift in the Bitlis Suture Zone was the result of a thin skinned, imbricated thrust and fold system. The imbricated thrust system sequence is composed of Late Cretaceous and younger strata. Shortening and vertical length estimates based on the direct comparison between the present-day balanced cross section and the reconstructed section from Late Cretaceous to Late Miocene time indicate 24.6 % shortening in the horizontal direction. Vertical thickening is greater in the north 36.56 % than in the south 11.18 % consistent with maintaining a wedge with a critical taper necessary for continued south directed thrusting during continent-continent collision. The interpreted structural evolution model from the restoration of geological structure will assist planning for petroleum exploration in this area. iv ACKNOWLEDGMENTS I am very grateful to Associate Professor Dr. John Hogan for his precious time to provide consultancy and reviewing this project. Also, I gratefully acknowledge Dr. Kelly Liu and Dr. Stephen Gao for helpful advice and all staff in the Department of Geology at Missouri University of Science and Technology, for their support during my study. I would like to acknowledge Turkish Petroleum Corporation for permission to use well data. Many thanks to all my friend for their encouragement and help with the administrative work involve in my project. This project is dedicated to my family whom I am grateful for their understanding, continue support and assistance while studying. v TABLE OF CONTENTS Page ABSTRACT ....................................................................................................................... iii ACKNOWLEDGMENTS ................................................................................................. iv LIST OF ILLUSTRATIONS ............................................................................................ vii SECTION 1. INTRODUCTION ...................................................................................................... 1 1.1. PURPOSE AND SCOPE .................................................................................... 1 1.2. GEOGRAPHIC LOCATION ............................................................................. 3 1.3. METHODS OF STUDY ..................................................................................... 3 1.4. PREVIOUS STUDIES........................................................................................ 5 1.5. GEOLOGICAL SETTING ................................................................................. 5 2. REGIONAL GEOLOGY ......................................................................................... 10 2.1. STRUCTURAL UNITS AND STRATIGRAPHY OF SOUTHEAST ANATOLIA ..................................................................................................... 10 2.1.1 The Arabian Platform .............................................................................. 12 2.1.1.1 Lower autochthonous succession. ...............................................12 2.1.1.2 Lower allochthonous units. .........................................................13 2.1.1.3 Upper autochthonous succession. ...............................................14 2.1.1.4 Upper allochthonous units. .........................................................14 2.1.2 The Zone of Imbrication .......................................................................... 14 2.1.3 The Nappe Zone. ..................................................................................... 15 2.2. SOUTHEAST ANATOLIA STRATIGRAPHY ALONG THE BALANCED CROSS SECTION ........................................................................................... 21 3. METHOD AND INVESTIGATION ....................................................................... 26 3.1. DATA ACQUISITION ..................................................................................... 26 3.2. FIELD WORK .................................................................................................. 26 3.3. THICKNESS OF STRATIGRAPHIC UNITS ................................................. 27 3.4. CONSTRUCTING CROSS SECTION ............................................................ 27 4. RESULTS ................................................................................................................. 31 vi 4.1. INTRODUCTION ............................................................................................ 31 4.2. RESULT FROM FIELD OBSERVATIONS ................................................... 31 4.3. BALANCED CROSS SECTION ..................................................................... 34 4.4. PALINSPASTIC RESTORATION .................................................................. 45 5. DISCUSSION .......................................................................................................... 48 5.1. BALANCED AND RESTORED CROSS SECTIONS FOR THE PAST AND PRESENT-DAY STRUCTURE OF THE BITLIS SUTURE ZONE .............. 48 5.1.1. Structural Style and Geometry. .............................................................. 48 5.1.2 Shortening of Study Area. ....................................................................... 49 5.1.3. Hydrocarbon Prospects. .......................................................................... 50 6. CONCLUSION AND RECOMMENDATION ....................................................... 52 6.1. CONCLUSION ................................................................................................. 52 6.2. RECOMMEDATION ....................................................................................... 53 APPENDICES A. PREVIOUS STUDIES ..................................................................................... 54 B. DIP-STRIKE MEASUREMENTS OF STUDY .............................................. 57 C. SATELITE IMAGE OF STUDY AREA ......................................................... 59 D. LOCATION OF MAJOR CONTACTS ........................................................... 61 BIBLIOGRAPHY ........................................................................................................ 63 VITA ............................................................................................................................ 65 vii LIST OF ILLUSTRATIONS Page Figure 1.1 Map showing location of the study area (Northeast of Adiyaman) Turkey, Google Earth, 2013). ..........................................................................................2 Figure 1.2 A flowchart detailing the steps needed to complete the study. ..........................4 Figure 1.3 (A) A simplified geologic map showing major plates and their boundary faults in the Eastern Mediterranean region (Tasgin et al., 2011) (B) Simplified neotectonic map showing major fault zones in the area surrounding and location of the study area, Adiyaman (Tasgin et al., 2011). ...6 Figure 1.4 Geologic map of the Southeast Anatolia (Yilmaz, 1993). ..................................9 Figure 2.1 Generalized (composite) stratigraphic section of the Arabian Platform in southeastern Anatolia (Modified after Yilmaz, 1993). ....................................11 Figure 2.2 Plate-tectonic models for the Mesozoic evolution of southeast Anatolia (Yilmaz, 1993). ................................................................................................17
Recommended publications
  • Resolving the Variscan Evolution of the Moldanubian Sector of The
    Journal of Geosciences, 52 (2007), 9–28 DOI: 10.3190/jgeosci.005 Original paper Resolving the Variscan evolution of the Moldanubian sector of the Bohemian Massif: the significance of the Bavarian and the Moravo–Moldanubian tectonometamorphic phases Fritz FINGER1*, Axel GERDEs2, Vojtěch JANOušEk3, Miloš RENé4, Gudrun RIEGlER1 1University of Salzburg, Division of Mineralogy, Hellbrunnerstraße 34, A-5020 Salzburg, Austria; [email protected] 2University of Frankfurt, Institute of Geoscience, Senckenberganlage 28, D-60054 Frankfurt, Germany 3Czech Geological Survey, Klárov 3, 118 21 Prague 1, Czech Republic 4Academy of Sciences, Institute of Rock Structure and Mechanics, V Holešovičkách 41, 182 09 Prague 8, Czech Republic *Corresponding author The Variscan evolution of the Moldanubian sector in the Bohemian Massif consists of at least two distinct tectonome- tamorphic phases: the Moravo–Moldanubian Phase (345–330 Ma) and the Bavarian Phase (330–315 Ma). The Mora- vo–Moldanubian Phase involved the overthrusting of the Moldanubian over the Moravian Zone, a process which may have followed the subduction of an intervening oceanic domain (a part of the Rheiic Ocean) beneath a Moldanubian (Armorican) active continental margin. The Moravo–Moldanubian Phase also involved the exhumation of the HP–HT rocks of the Gföhl Unit into the Moldanubian middle crust, represented by the Monotonous and Variegated series. The tectonic emplacement of the HP–HT rocks was accompanied by intrusions of distinct magnesio-potassic granitoid melts (the 335–338 Ma old Durbachite plutons), which contain components from a strongly enriched lithospheric mantle source. Two parallel belts of HP–HT rocks associated with Durbachite intrusions can be distinguished, a western one at the Teplá–Barrandian and an eastern one close to the Moravian boundary.
    [Show full text]
  • Balkatach Hypothesis: a New Model for the Evolution of the Pacific, Tethyan, and Paleo-Asian Oceanic Domains
    Research Paper GEOSPHERE Balkatach hypothesis: A new model for the evolution of the Pacific, Tethyan, and Paleo-Asian oceanic domains 1,2 2 GEOSPHERE, v. 13, no. 5 Andrew V. Zuza and An Yin 1Nevada Bureau of Mines and Geology, University of Nevada, Reno, Nevada 89557, USA 2Department of Earth, Planetary, and Space Sciences, University of California, Los Angeles, California 90095-1567, USA doi:10.1130/GES01463.1 18 figures; 2 tables; 1 supplemental file ABSTRACT suturing. (5) The closure of the Paleo-Asian Ocean in the early Permian was accompanied by a widespread magmatic flare up, which may have been CORRESPONDENCE: avz5818@gmail .com; The Phanerozoic history of the Paleo-Asian, Tethyan, and Pacific oceanic related to the avalanche of the subducted oceanic slabs of the Paleo-Asian azuza@unr .edu domains is important for unraveling the tectonic evolution of the Eurasian Ocean across the 660 km phase boundary in the mantle. (6) The closure of the and Laurentian continents. The validity of existing models that account for Paleo-Tethys against the southern margin of Balkatach proceeded diachro- CITATION: Zuza, A.V., and Yin, A., 2017, Balkatach hypothesis: A new model for the evolution of the the development and closure of the Paleo-Asian and Tethyan Oceans criti- nously, from west to east, in the Triassic–Jurassic. Pacific, Tethyan, and Paleo-Asian oceanic domains: cally depends on the assumed initial configuration and relative positions of Geosphere, v. 13, no. 5, p. 1664–1712, doi:10.1130 the Precambrian cratons that separate the two oceanic domains, including /GES01463.1. the North China, Tarim, Karakum, Turan, and southern Baltica cratons.
    [Show full text]
  • The Geology of England – Critical Examples of Earth History – an Overview
    The Geology of England – critical examples of Earth history – an overview Mark A. Woods*, Jonathan R. Lee British Geological Survey, Environmental Science Centre, Keyworth, Nottingham, NG12 5GG *Corresponding Author: Mark A. Woods, email: [email protected] Abstract Over the past one billion years, England has experienced a remarkable geological journey. At times it has formed part of ancient volcanic island arcs, mountain ranges and arid deserts; lain beneath deep oceans, shallow tropical seas, extensive coal swamps and vast ice sheets; been inhabited by the earliest complex life forms, dinosaurs, and finally, witnessed the evolution of humans to a level where they now utilise and change the natural environment to meet their societal and economic needs. Evidence of this journey is recorded in the landscape and the rocks and sediments beneath our feet, and this article provides an overview of these events and the themed contributions to this Special Issue of Proceedings of the Geologists’ Association, which focuses on ‘The Geology of England – critical examples of Earth History’. Rather than being a stratigraphic account of English geology, this paper and the Special Issue attempts to place the Geology of England within the broader context of key ‘shifts’ and ‘tipping points’ that have occurred during Earth History. 1. Introduction England, together with the wider British Isles, is blessed with huge diversity of geology, reflected by the variety of natural landscapes and abundant geological resources that have underpinned economic growth during and since the Industrial Revolution. Industrialisation provided a practical impetus for better understanding the nature and pattern of the geological record, reflected by the publication in 1815 of the first geological map of Britain by William Smith (Winchester, 2001), and in 1835 by the founding of a national geological survey.
    [Show full text]
  • The Mio-Eugeosynclinal Thrust Interface and Related Petroleum Implications in the Sason-Baykan Area, Southeast Turkey
    Scholars' Mine Doctoral Dissertations Student Theses and Dissertations 1972 The mio-eugeosynclinal thrust interface and related petroleum implications in the Sason-Baykan Area, Southeast Turkey Ismail Özkaya Follow this and additional works at: https://scholarsmine.mst.edu/doctoral_dissertations Part of the Geology Commons Department: Geosciences and Geological and Petroleum Engineering Recommended Citation Özkaya, Ismail, "The mio-eugeosynclinal thrust interface and related petroleum implications in the Sason- Baykan Area, Southeast Turkey" (1972). Doctoral Dissertations. 198. https://scholarsmine.mst.edu/doctoral_dissertations/198 This thesis is brought to you by Scholars' Mine, a service of the Missouri S&T Library and Learning Resources. This work is protected by U. S. Copyright Law. Unauthorized use including reproduction for redistribution requires the permission of the copyright holder. For more information, please contact [email protected]. THE MIO- EUGEOSYNCLINAL THRUST INTERFACE AND RELATED PETROLEUM IMPLICATIONS IN THE SASON-BAYKAN AREA, SOUTHEAST TURKEY by ISMAIL OZKAYA, 194 A DISSERTATION Presented to the Faculty of the Graduate School of the UNIVERSITY OF MISSOURI-ROLLA In Partial Fulfi I lment of the Requirements for the Degree DOCTOR OF PHILOSOPHY in GEOLOGY 1972 p ·' ~&IA-~f ~ i i ABSTRACT A detailed investigation of the stratigraphy, structure and petroleum geology of the Sason-Baykan region in 600 square km area of the thrust belt of southeast Turkey was completed at a scale 1: 25 000. Geosynclinal sediments within the area were redated. Results of field study indicate a massive plate of metamorphic rocks and crystal I ine limestones was thrust southward over geosynclinal sediments. These in turn were thrust over the southern marginal basin deposits.
    [Show full text]
  • Imaging the Upper Mantle Beneath Turkey and Surrounding Regions
    IMAGING THE UPPER MANTLE BENEATH TURKEY AND SURROUNDING REGIONS by Ahu Kömeç Mutlu B.Sc., Geophysical Engineering, İstanbul University, 2000 M.Sc., Geophysical Engineering, Boğaziçi University, 2005 Submitted to the Kandilli Observatory and Earthquake Research Institute in partial fulfillment of the requirements for the degree of Doctor of Philosophy Graduate Program in Geophysics Department Boğaziçi University 2012 ii IMAGING THE UPPER MANTLE BENEATH TURKEY AND SURROUNDING REGIONS APPROVED BY: Prof. Dr. Hayrullah Karabulut ............................. (Thesis Supervisor) Prof. Dr. Niyazi Türkelli ............................. Assoc. Prof. Dr. Nurcan Meral Özel … ........................ Assist. Prof. Ali Özgün Konca ............................. Prof. Dr. Argun Kocaoğlu ............................. (İ.T.U.) DATE OF APPROVAL: 16.02.2012 iii To my father İlker Kömeç, iv ACKNOWLEDGEMENTS I would like to express my appreciation to my academic advisor Prof. Hayrullah Karabulut for his guidance and encouragement. I am grateful to him for his endless support and patience during my PhD study. It is always pleasure to be one of his students and work with him. Thanks to the Kandilli Observatory and Earthquake Research Institute, National Earthquake Monitoring Center (KOERI-NEMC), International Seismological Centre (ISC), European–Mediterranean Seismological Centre (EMSC), Incorporated Research Institutions for Seismology (IRIS) and GEOFON Seismic Network for providing earthquake catalog and seismic data. I would like to thank the Department of Geophysics for providing environment for education and research. Thanks also to Dr. Anne Paul from the Institute des Sciences de la Terre (France) for providing the SIMBAAD data (funded by ANR France, contract 06-BLAN-0317). She also provided guidance on shear wave splitting analysis. I would like to thank Dr. Andreas Wüstefeld for his MATLAB interface, which facilitates the processing of shear wave splitting observations.
    [Show full text]
  • 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.
    [Show full text]
  • Pre-Mesozoic Geology of Saxo-Thuringia from the Cadomian Active Margin to the Variscan Orogen
    GEOLOGICA CARPATHICA, FEBRUARY 2011, 62, 1, 42 BOOK REVIEW Pre-Mesozoic Geology of Saxo-Thuringia From the Cadomian Active Margin to the Variscan Orogen Editors: ULF LINNEMANN & ROLF L. ROMER 26–28 April 2010 2010. Schweizerbart Science Publishers, Stuttgart. 488 pages, 190 figures, 6 tables, 1 Sheet Map, 1 DVD, 1 foldout, 25x 17 cm, 1400 g. Language: English ISBN 978-3-510-65259-4, bound, price: 84.90 EUR The monographic work is a summary of results of a wider team of authors, who have contributed to the five dominant Parts, each of which consists of several Chapters focused on individual problems of the Saxo-Thuringian Region, its geological structure and its development in time and space. It is a classical analysis of the development of the Pre-Mesozoic stage from the Cadomian Active Margin to the Variscan Orogene. Saxo-Thuringia represents a very important region displaying development of the Variscides in one part of the Pangea supercontinent. The first chapter of the first part (Introduction) of the book is absolutely devoted to the location of this region of Saxo-Thuringia in the context of the Pangea supercontinent, followed by detailed recapitulation of the geological maps and results from geological mapping in historical survey from oldest documents to almost present- day works, which are well preserved and represent for the reader the classical and modern shool of regional geology of this region. The third chapter of this part completely untraditionally, but in a very interesting way shows the region of Saxo- Thuringia from the point of view of geochemical potential.
    [Show full text]
  • Collision Orogeny
    Downloaded from http://sp.lyellcollection.org/ by guest on October 6, 2021 PROCESSES OF COLLISION OROGENY Downloaded from http://sp.lyellcollection.org/ by guest on October 6, 2021 Downloaded from http://sp.lyellcollection.org/ by guest on October 6, 2021 Shortening of continental lithosphere: the neotectonics of Eastern Anatolia a young collision zone J.F. Dewey, M.R. Hempton, W.S.F. Kidd, F. Saroglu & A.M.C. ~eng6r SUMMARY: We use the tectonics of Eastern Anatolia to exemplify many of the different aspects of collision tectonics, namely the formation of plateaux, thrust belts, foreland flexures, widespread foreland/hinterland deformation zones and orogenic collapse/distension zones. Eastern Anatolia is a 2 km high plateau bounded to the S by the southward-verging Bitlis Thrust Zone and to the N by the Pontide/Minor Caucasus Zone. It has developed as the surface expression of a zone of progressively thickening crust beginning about 12 Ma in the medial Miocene and has resulted from the squeezing and shortening of Eastern Anatolia between the Arabian and European Plates following the Serravallian demise of the last oceanic or quasi- oceanic tract between Arabia and Eurasia. Thickening of the crust to about 52 km has been accompanied by major strike-slip faulting on the rightqateral N Anatolian Transform Fault (NATF) and the left-lateral E Anatolian Transform Fault (EATF) which approximately bound an Anatolian Wedge that is being driven westwards to override the oceanic lithosphere of the Mediterranean along subduction zones from Cephalonia to Crete, and Rhodes to Cyprus. This neotectonic regime began about 12 Ma in Late Serravallian times with uplift from wide- spread littoral/neritic marine conditions to open seasonal wooded savanna with coiluvial, fluvial and limnic environments, and the deposition of the thick Tortonian Kythrean Flysch in the Eastern Mediterranean.
    [Show full text]
  • Crystalline Complexes in the Southern Parts O.F the Bohemian Massif and in the Eastern Alps by G
    INTERNATIONAL GEOLOGICAL CONGRESS XXIII SESSION PRAGUE 1968 Guide to Excursion 32 C Austria Crystalline Complexes in the Southern Parts o.f the Bohemian Massif and in the Eastern Alps by G. Frasl, H. G. Scharbert, H. Wieseneder PUBLISHED BY THE GEOLOGICAL SURVEY OF AUSTRIA Excursion 32 C / Aug. 31.-Sept. 3, 1968 Excursion Leaders and Authors of the Excursion-guide: G. FRASL Universität Salzburg, Institut für Geologie und Paläontologie - Salzburg, Porsdie­ straße 8. H. G. ScHARBER T Universität Wien, Mineralogisch-Petrographisches Institut - Wien I, Dr.-Karl-Lueger­ ring 1. H. WIESENEDER Universität Wien, Mineralogisch-Petrographisches Institut - Wien 1, Dr.-Karl-Lueger­ ring 1. All rights reserved. Copyright, 1968, © by Geologische Bundesanstalt, Wien III. Printed in Austria. Contents I. The Bohernian Massif in Austria, Moldanubian Zone. H. G. ScHARBERT (First day) . 5 Introduction . 5 The excursion (Stop 1/1-stop I/6) 9 II. The Bohemian Massif in Austria, Moravian Zone. G. FRASL (Second day) . 13 General remarks . 13 The excursion (Stop II/1-stop II/9) 17 III. The eastern End of the Central Alps. H. WIESENEDER (Third and fo*th day) 25 General geology of the area . 25 The Wechsel unit . 25 The "grobgneiss" formation . 26 Permo-Mesozoic . 28 Metamorphism in the Semmering-Wechsel area . 30 The excursion (Stop III/1-stop III/11) . 30 Selected literature within ead1 article 1 (First day) The Bohemian Massif in Austria The Moldanubian Zone By H. G. ScHARBERT With 1 figure Introduction The Bohemian Massif is a deeply eroded cratogenic block having re­ ceived its last tectonic coining during the Variscian orogeny.
    [Show full text]
  • 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.
    [Show full text]
  • Ages of Detrital Zircons
    Elsevier Editorial System(tm) for Precambrian Research Manuscript Draft Manuscript Number: Title: AGES OF DETRITAL ZIRCONS (U/Pb, LA-ICP-MS) FROM THE LATEST NEOPROTEROZOIC - MIDDLE CAMBRIAN(?) ASHA GROUP AND EARLY DEVONIAN TAKATY FORMATION, THE SOUTH- WESTERN URALS: A TEST OF AN AUSTRALIA-BALTICA CONNECTION WITHIN RODINIA Article Type: SI:Precambrian Supercontinents Keywords: Urals, Detrital Zircon, Rodinia, Ediacaran, Baltica Corresponding Author: Prof. Nikolay Borisovich Kuznetsov, Ph.D. Corresponding Author's Institution: Geological Institute of Russian Academy of Science First Author: Nikolay B Kuznetsov, Ph.D. Order of Authors: Nikolay B Kuznetsov, Ph.D.; Josef G Meert, Ph.D.; Tatiana V Romanyuk, Ph.D. Abstract: Results from U/Pb-dating of detrital zircons (dZr) from sandstones of the Basu and Kukkarauk Fms. (Asha Group) of Ediacaran-Middle Cambrian(?) age along with the results obtained from the Early Devonian Takaty Fm. are presented. The age of the Asha Group is traditionally labeled as Upper Vendian in the Russian stratigraphic chart that overlaps with the Ediacaran in the International stratigraphic chart. The dZr whose ages fall within the age-interval of (500-750 Ma) are common in the Basu and Kukkarauk Fm. These ages are typical for crystalline complexes in the Pre- Uralides-Timanides orogen. The identification of zircons with this age range agrees with commonly adopted interpretations for the depositional origin of the Asha Group as a molasse resulting from the erosion of that orogenic belt. Based on the estimates of the youngest ages of dZr along with the tentative identification of inarticulate brachiopods in the Kukkarauk Fm., it appears that the upper part of the Asha Group may extend into the Middle Cambrian.
    [Show full text]
  • The Geodynamics of the Aegean and Anatolia: Introduction
    Downloaded from http://sp.lyellcollection.org/ by guest on September 27, 2021 The geodynamics of the Aegean and Anatolia: introduction T. TAYMAZ1, Y. YILMAZ2 & Y. DILEK3 1Department of Geophysical Engineering,˙ Istanbul Technical University, Maslak, TR–34469,˙ Istanbul, Turkey (e-mail: [email protected]) 2Kadir Has University, Fatih, I˙stanbul, Turkey 3Department of Geology, Miami University, Oxford, OH 45056, USA The complexity of the plate interactions and and volcanism in Anatolia and the Aegean region associated crustal deformation in the Eastern (Taymaz et al. 2004). Mediterranean region is reflected in many destruc- tive earthquakes that have occurred throughout Regional synthesis its recorded history, many of which are well documented and intensively studied. The Eastern Given its location in the Alpine–Himalayan Mediterranean region, including the surrounding orogenic belt, and at the collisional boundary areas of western Turkey and Greece, is indeed one between Gondwana and Laurasia, the geological of the most seismically active and rapidly deform- history of the Aegean region and Anatolia involves ing regions within the continents (Fig. 1). Thus, the Mesozoic–Cenozoic closure of several Neo- the region provides a unique opportunity to tethyan oceanic basins, continental collisions and improve our understanding of the complexities of subsequent post-orogenic processes (e.g. Sengo¨r continental tectonics in an actively collisional & Yılmaz 1981; Bozkurt & Mittwede 2001; Okay orogen. The major scientific observations from et al. 2001; Dilek & Pavlides 2006; Robertson & this natural laboratory have clearly been helping Mountrakis 2006). The opening of oceanic branches us to better understand the tectonic processes in of Neotethys commenced in the Triassic and active collision zones, the mode and nature of they closed during the Late Cretaceous to Eocene continental growth, and the causes and distribution time interval.
    [Show full text]