DOCSLIB.ORG

Devonian in Turkey - a Review

Total Page：16

File Type：pdf, Size：1020Kb

Download full-text PDF Read full-text
Devonian in Turkey - a Review See discussions, stats, and author profiles for this publication at: https://www.researchgate.net/publication/250166975 Devonian in Turkey - A review Article in Geologica Carpathica · June 2010 DOI: 10.2478/v10096-010-0014-3 CITATIONS READS 27 1,025 2 authors: M. Namık Yalçın Isak yılmaz Istanbul University Istanbul University 89 PUBLICATIONS 1,087 CITATIONS 11 PUBLICATIONS 126 CITATIONS SEE PROFILE SEE PROFILE Some of the authors of this publication are also working on these related projects: Silurian / Devonian Boundary View project Thermal Analysis of Source Rocks for characterization and decontamination View project All content following this page was uploaded by Isak yılmaz on 13 May 2015. The user has requested enhancement of the downloaded file. GEOLOGICA CARPATHICA, JUNE 2010, 61, 3, 235—253 doi: 10.2478/v10096-010-0014-3 Devonian in Turkey – a review M. NAMIK YALÇIN and ISAK YILMAZ Istanbul University, Faculty of Engineering, Department of Geological Engineering, TR-34850 Avcôlar-Istanbul, Turkey; [email protected]; [email protected] (Manuscript received August 13, 2009; accepted in revised form December 11, 2009) Abstract: The Devonian Period is represented in Turkey by almost complete non-metamorphic sections of more than 1000 meters, which exhibit varying lithofacial associations. They are parts of thick Paleozoic sedimentary successions in the Pontides, Taurides and Arabian Plate. The tectonic setting and the paleogeographical origin of these terranes is different. Therefore, the litho- and biostratigraphy and facies characteristics of these Devonian successions would enable a comparison and a paleogeographical assignment of these tectono-stratigraphic units. Devonian successions of the Arabian Plate and of the Taurides are represented by facies associations ranging from tidal flat to a deep shelf. Whereas, those of the Istanbul and Çamdag-Zonguldak˘ areas in the Pontides by a deepening upward sequence from a shallow shelf into a basin and a stable shelf, respectively. The Devonian of the Arabian Plate and the Taurides can surely be assigned to Gondwana. A Peri-Gondwanan (Avalonian) setting is suggested for the paleogeographic position of the Devonian of the Pontides. Key words: Devonian, Turkey, paleogeography, depositional environment, biostratigraphy, lithostratigraphy. Introduction ous authors from north to south as Pontides, Sakarya Conti- nent, Menderes and Kôrehir Blocks, Taurides and the Arabi- The geological and tectonic frame of Turkey, located in the an Plate (Fig. 1), generally represent continental terranes Alpine-Himalayan Orogenic Belt, is mainly formed by the separated by suture zones. The suture zones are in general Alpine orogeny. Accordingly, a number of E-W trending composed of ophiolitic and volcanic rocks of oceanic origin tectono-stratigraphic units are defined, which consist of ter- (Ketin 1966; engör & Yôlmaz 1981; Göncüoglu˘ 1997). Not ranes of different tectonic settings ranging from oceanic ba- only the tectonic setting of these terranes is different, but sins to active and passive continental margins. The also the geological age of the incorporated units reflects a tectono-stratigraphic units as distinguished by many previ- wide spectrum from Infra-Cambrian to Tertiary. Fig. 1. Tectonic map of Turkey showing the major blocks/terranes and the bounding suture zones. Distribution of Devonian succesions are also shown and those, which are discussed in detail, are indicated by numbers. 1 – Istanbul Zone, 2 – Çamda˘g area, 3 – Eastern Taurides, 4 – Cen- tral Taurides, 5 – Aladag˘ and Bolkardag˘ Units in Taurides, 6 – Western Taurides, 7 – Karaburun area, 8 – Hakkari area of Arabian Plate, 9 – Hazro area of Arabian Plate, 10 – Amanos area of Arabian Plate. (Modified from engör & Yôlmaz 1981 and Elmas & Yi˘gitba 2001.) www.geologicacarpathica.sk 236 YALÇIN and YILMAZ Devonian units of different litho-types and of different quently, the Silurian/Devonian (S/D) boundary has to be lo- paleogeographic origin are parts of thick Paleozoic sedimen- cated within the uppermost part of the Dada Formation. tary successions of the Pontides, Taurides and Arabian Plate. Some recent efforts to localize the S/D boundary in Hazro area Some minor occurrences of sedimentary Devonian are also along the measured stratigraphic section Fetlika and in the reported from the Karaburun area and Aegean Islands in well Fetlika-1 showed that the boundary cannot be localized westernmost Turkey relatively early by Ktenas (1925) only by palinomorphs (Mann et al. 2001; Kranendonck 2004; (Fig. 1). This region was studied then by many scientists be- Brocke et al. 2004). In the Amanos area and in the Hakkari cause of the complicated stratigraphy and tectonics (Höll area, respectively to the west and east of Southeastern Anato- 1966; Lehnert-Thiel 1969; Konuk 1979; Erdogan˘ et al. 1990; lia, Silurian is not represented (Yôlmaz & Duran 1997). Con- Kozur 1995; Kaya & Rezsu 2000; Rosselet & Stampfli sequently, Upper Devonian Yôg˘ ônlô and Köprülü Formations 2002; Eren et al. 2004; Çakmakoglu˘ & Bilgin 2006; Okay et lie with an angular unconformity on the Ordovician Bedinan al. 2006). A relatively thick succession bearing also Devo- Formation (Fig. 2). nian units is interpreted by Çakmakoglu˘ & Bilgin (2006) as autochthonous. The same succession was considered by Ko- Litho- and biostratigraphy of the Devonian in the Hazro zur (1995, 1997) and Rosselet et al. (2003) as an allochtho- area nous sedimentary melange. Most recent studies however showed that Devonian rocks in the Karaburun area are al- The Devonian succession in the Hazro area north of Di- lochthonous blocks and olistolith within the Carboniferous yarbakôr (Fig. 1) is named as the Diyarbakôr Group and is flysch (Robertson & Ustaömer 2009). composed of the Dada, Hazro and Kayayolu Formations Metamorphic Devonian units are reported from parts of the (Bozdogan˘ et al. 1987) (Fig. 2). The Kayayolu Formation is Central Anatolian Massif, Menderes Massif in western Turkey only encountered in wells, whereas outcrops of Dada and and in eastern Turkey from the Bitlis Massif (Göncüoglu˘ & Hazro Formations are represented in the so-called Hazro High. Turhan 1983). The total thickness of these units on the surface varies be- The aim of this paper is to give an overview of the Turkish tween 70 and 217 m (Sungurlu 1974; Bozdogan˘ et al. 1987). autochthonous and non-metamorphic Devonian. Hereby, In the subsurface they can be up to 500 m thick (Bozdogan˘ et based mainly on the data obtained from previous studies, the al. 1987). Within the Dada Formation, three subunits (mem- geographical distribution, general geological setting, litho- bers) are distinguished based on different lithological compo- and biostratigraphy and facies characteristics of these Devo- sition, which are reflected in log characteristics (Bozdogan˘ et nian successions will be addressed on the basis of the tectono- al. 1987). The Dada I Member consists of dark coloured, or- stratigraphic subdivision of Turkey. ganic rich shales with some limestone interbeds; the Dada II Member is composed of similar shales alternating with some sandstones and the Dada III Member consists of an alterna- Devonian of the Arabian Plate in Southeastern tion of sandstones, marls and calcareous siltstones. The Dada Anatolia Formation lies unconformably on the Middle—Upper Ordovi- cian Bedinan Formation and is overlain conformably by the The Devonian of the Arabian Plate is represented in South- Devonian Hazro Formation (Bozdogan˘ et al. 1987; Perinçek et eastern Anatolia by sedimentary sequences observed from al. 1991). The Dada Formation is rich in fossils of palinomor- west to east in the Amanos Mountains, Hazro High and phs, brachiopods, bryozoans, graptolites, conodonts, crinoids, Hakkari area. Furthermore, they are encountered in some corals and ostracods. Fossil assemblages reported by different wells around the Diyarbakôr area (Fig. 1). The Devonian of the authors (Çoruh et al. 1997 and references there in) from the northerly located Hazro area is represented by Lower to Upper middle and upper parts of the Dada Formation are listed in Devonian, while the Devonian of the other two regions con- the Appendix. According to these fossils and to detailed pali- sists of only Upper Devonian (Bozdogan˘ et al. 1987; Yôlmaz nological studies by Bozdogan˘ et al. (1987), Ertug˘ et al. & Duran 1997). But, in both geological settings the underlying (1998), Brocke et al. (2004), Bozdogan˘ et al. (2005) a Late units are similar. A thick Pre-Cambrian to Upper Ordovician Silurian—Early Devonian age is assigned to the Dada Forma- continuous sedimentary sequence forms the pre-Devonian tion. As mentioned before, the exact location of Silurian/De- basement in both settings (Fig. 2). The Silurian-Devonian vonian boundary is still not determined. The Dada Formation Dada Formation, outcrops only in Diyarbakôr in the Hazro was deposited on a restricted inner shelf, which was devel- High and is also encountered in some wells there. According oped on the irregular paleotopography of the eroded Bedinan to observations and records in Kayayolu-2 well this unit was Formation. The respective shelf became shallower and was deposited after a regional break in sedimentation (Bozdogan˘ et gradually converted to a tidal flat towards the top of the se- al. 1987; Yôlmaz & Duran 1997). Therefore it is inferred, that quence (Yôlmaz & Duran 1997). the Dada Formation lies with an angular unconformity on the The following Hazro Formation consists in general of an al-
Load more

Recommended publications
  • 2018 YILI FAALİYET RAPORU.Pdf
    SAKARYA İL TARIM ve ORMAN MÜDÜRLÜĞÜ 2018 YILI FAALİYET ÖZETİ SAKARYA ARALIK-2018 1 SAKARYA İL TARIM VE ORMAN MÜDÜRLÜĞÜ İl ve İlçe Müdürlükleri Personel Durumu Sakarya İl Tarım ve Orman Müdürlüğü 1 İl Müdürü, 3 İl Müdür Yardımcısı, 8 Şube Müdürü, 16 İlçe Müdürü yönetiminde toplam 516 personelle hizmetlerini yürütmektedir. Su Ürünleri SAKARYA İL TARIM VE ORMAN Ziraat Vet.Sağ. Ziraat Mühendisi Gıda Mühendisi Müh.- Balıkçılık Veteriner Hekim Teknis/Tekn. Tekns/Tekn. MÜDÜRLÜĞÜ Tek.Müh. Norm 4/A 4/B Norm 4/A 4/B Norm 4/A Norm 4/A 4/B Norm 4/A Norm 4/A ARAZİ TOP. VE TARIM.ALT YAPI ŞB.MD. 14 9 1 - 0 0 - 0 - 0 0 3 2 - 0 ÇAYIR, MERA VE YEM BİT.ŞB. 3 0 - 0 0 - 0 - 0 0 0 - 0 BİTKİSEL ÜRETİM VE SAĞ.ŞB.MD. 26 13 2 - 0 0 - 0 - 0 0 5 3 - 0 HAYVAN SAĞLIĞI YETİŞ.ŞB.MD. 4 0 0 - 0 0 - 0 19 8 6 - 0 5 3 BALIKÇILIK VE SU ÜRÜNLERİ ŞB.MD. - 0 0 - 0 0 8 7 1 0 0 - 0 - 0 KOORDİNASYON VE TAR.VER.ŞB.MD. 5 6 0 - 0 0 - 0 - 0 0 5 2 - 0 KIRSAL KALKINMA VE ÖRGÜT.ŞB.MD. 16 6 0 - 0 0 - 0 2 1 0 4 2 - 0 GIDA VE YEM ŞB.MD. 13 1 1 31 5 5 - 0 19 7 2 - 0 - 0 İL MÜDÜRLÜĞÜ TOPLAMI 78 38 4 31 5 5 8 7 41 16 8 17 9 5 3 ADAPAZARI 16 8 3 6 5 1 1 0 19 11 1 6 2 4 2 AKYAZI 12 4 4 2 0 1 2 0 12 6 0 5 1 3 2 ARİFİYE 4 4 1 1 1 0 - 1 2 2 0 2 2 2 1 ERENLER 9 7 1 2 4 0 - 0 9 6 1 6 2 2 0 FERİZLİ 9 1 3 1 0 1 - 0 5 1 0 6 1 3 0 GEYVE 15 2 5 1 0 1 - 0 8 3 3 9 1 3 2 HENDEK 15 8 3 2 0 1 2 0 13 8 1 5 2 3 1 KARAPÜRÇEK 4 3 0 - 0 0 - 0 2 2 1 2 0 2 0 KARASU 19 4 3 2 1 1 3 2 9 5 2 7 1 3 2 KAYNARCA 12 6 3 - 0 0 1 1 11 5 2 7 0 3 2 KOCAALİ 18 3 4 1 0 0 1 0 4 2 1 5 1 2 2 PAMUKOVA 9 3 4 1 0 1 1 0 5 4 1 5 2 3 1 SAPANCA
    [Show full text]
  • Palaeoenvironmental Interpretation of the Triassic Sandstones of Scrabo
    PALAEOENVIRONMENTAL INTERPRETATION OF THE TRIASSIC SANDSTONES OF SCRABO, COUNTY DOWN, NORTHERN IRELAND: ICHNOLOGICAL AND SEDIMENTOLOGICAL STUDIES INDICATING A MIXED FLUVIATILE-AEOLIAN SUCCESSION JAMES O. BUCKMAN, PHILIPS. DOUGHTY,MICHAEL J. BENTON and ANDREW J. JERAM (Received 19 May 1997) Abstract The Sherwood Sandstone Group at Scrabo, Co. Down, NorthernIreland, has been variously interpretedas aeolian or fluviatile. The sedimentological and ichnological data show that these sandstone-dominatedfacies were deposited within a mixed fluviatile-aeolian regime, in which fluviatile processes were responsible for the majorityof the preservedsedimentary sequence. The sequence contains a moderately diverse non-marine ichnofauna comprising the invertebratetrace fossils Biformites, Cruziana/Rusophycus(Isopodichnus), Herpystezoum(Unisulcus), Planolites, 'small arthropodtrackways', 'large arthropodtrackways' (cf. in part Paleohelcura), and the vertebrate trace fossil Chirotherium? (as well as a number of other, presently unnamed, vertebrate footprints). The recorded ichnofauna greatly increases that previously known from the Irish Triassic, comparesfavourably with that from the rest of Europe, and representsthe only known Irish locality for reptiliantrackways. Introduction north-east, are exposed at Scrabo Hill (Charlesworth 1963). Several Palaeogene The Sherwood Sandstone Group (Triassic) dolerite dykes and sills are exposed at the in north-eastIreland comprises part of a thick southern end of the hill, and these form a sequence of non-marine sediments, with a resistant cap that has shielded the sandstones maximum thickness of 1850m (Parnell et al. against removal by ice during the last 1992), which are rarely exposed and known glaciations. mostly from borehole data. At Scrabo (Fig. 1) Various environmental interpretationshave the Sherwood SandstoneGroup occurs within a been made of the Scrabo succession. The deep trough of Carboniferousto Triassic age succession has been interpretedas representing (Parnell et al.
    [Show full text]
  • Copertina Guida Ai TRILOBITI V3 Esterno
    Enrico Bonino nato in provincia di Bergamo nel 1966, Enrico si è laureato in Geologia presso il Dipartimento di Scienze della Terra dell'Università di Genova. Attualmente risiede in Belgio dove svolge attività come specialista nel settore dei Sistemi di Informazione Geografica e analisi di immagini digitali. Curatore scientifico del Museo Back to the Past, ha pubblicato numerosi volumi di paleontologia in lingua italiana e inglese, collaborando inoltre all’elaborazione di testi e pubblicazioni scientifiche a livello nazonale e internazionale. Oltre alla passione per questa classe di artropodi, i suoi interessi sono orientati alle forme di vita vissute nel Precambriano, stromatoliti, e fossilizzazioni tipo konservat-lagerstätte. Carlo Kier nato a Milano nel 1961, Carlo si è laureato in Legge, ed è attualmente presidente della catena di alberghi Azul Hotel. Risiede a Cancun, Messico, dove si dedica ad attività legate all'ambiente marino. All'età di 16 anni, ha iniziato una lunga collaborazione con il Museo di Storia Naturale di Milano, ed è a partire dal 1970 che prese inizio la vera passione per i trilobiti, dando avvio a quella che oggi è diventata una delle collezioni paleontologiche più importanti al mondo. La sua instancabile attività di ricerca sul terreno in varie parti del globo e la collaborazione con professionisti del settore, ha permesso la descrizione di nuove specie di trilobiti ed artropodi. Una forte determinazione e la costruzione di un nuovo complesso alberghiero (AZUL Sensatori) hanno infine concretizzzato la realizzazione
    [Show full text]
  • Reassignment of Vertebrate Ichnotaxa from the Upper Carboniferous 'Fern
    Reassignment of vertebrate ichnotaxa from the Upper Carboniferous ‘Fern Ledges’, Lancaster Formation, Saint John, New Brunswick, Canada MATTHEW R. STIMSON1,2*, RANDALL F. MILLER1, AND SPENCER G. LUCAS3 1. Steinhammer Palaeontology Laboratory, New Brunswick Museum, Saint John, New Brunswick E2K 1E5, Canada 2. New Brunswick Geological Surveys Branch, Department of Energy and Mines, Fredericton, New Brunswick E3B 5H1, Canada 3. New Mexico Museum of Natural History and Science, Albuquerque, New Mexico 87104, USA *Corresponding author <[email protected]> Date received: 14 April 2015 ¶ Date accepted: 04 September 2015 ABSTRACT Vertebrate ichnotaxa described by George Frederic Matthew in 1910 from the Upper Carboniferous (Lower Pennsylvanian) ‘Fern Ledges’ of Saint John, New Brunswick, were dismissed as dubious trackways by previous authors. Thus, three new ichnospecies Matthew described appeared in the 1975 Treatise on Invertebrate Paleontology as “unrecognized or unrecognizable” and were mostly forgotten by vertebrate ichnologists. These traces include Hylopus (?) variabilis, Nanopus (?) vetustus and Bipezia bilobata. One ichnospecies, Hylopus (?) variabilis, here is retained as a valid tetrapod footprint ichnotaxon and reassigned to the ichnogenus Limnopus as a new combination, together with other poorly preserved specimens Matthew labeled, but never described. Nanopus (?) vetustus and Bipezia bilobata named by Matthew in the same paper, have been reexamined and remain as nomina dubia. RÉSUMÉ Les ichnotaxons vertébrés de Fern Ledges du Carbonifère supérieur (Pennsylvanien inférieur) de Saint John, au Nouveau-Brunswick, décrits par George Frederic Matthew en 1910 avaient été rejetés par des auteurs précédents les considérant comme des séries de traces douteuses. Trois nouvelles ichnoespèces décrites par Matthew sont ainsi appa- rues dans le Treatise on Invertebrate Paleontology (Traité sur la paléontologie des invertébrés) de 1975 à titre d’espèces « non identifiées ou non identifiables » et ont principalement été laissées aux ichnologues des vertébrés.
    [Show full text]
  • 001-012 Primeras Páginas
    PUBLICACIONES DEL INSTITUTO GEOLÓGICO Y MINERO DE ESPAÑA Serie: CUADERNOS DEL MUSEO GEOMINERO. Nº 9 ADVANCES IN TRILOBITE RESEARCH ADVANCES IN TRILOBITE RESEARCH IN ADVANCES ADVANCES IN TRILOBITE RESEARCH IN ADVANCES planeta tierra Editors: I. Rábano, R. Gozalo and Ciencias de la Tierra para la Sociedad D. García-Bellido 9 788478 407590 MINISTERIO MINISTERIO DE CIENCIA DE CIENCIA E INNOVACIÓN E INNOVACIÓN ADVANCES IN TRILOBITE RESEARCH Editors: I. Rábano, R. Gozalo and D. García-Bellido Instituto Geológico y Minero de España Madrid, 2008 Serie: CUADERNOS DEL MUSEO GEOMINERO, Nº 9 INTERNATIONAL TRILOBITE CONFERENCE (4. 2008. Toledo) Advances in trilobite research: Fourth International Trilobite Conference, Toledo, June,16-24, 2008 / I. Rábano, R. Gozalo and D. García-Bellido, eds.- Madrid: Instituto Geológico y Minero de España, 2008. 448 pgs; ils; 24 cm .- (Cuadernos del Museo Geominero; 9) ISBN 978-84-7840-759-0 1. Fauna trilobites. 2. Congreso. I. Instituto Geológico y Minero de España, ed. II. Rábano,I., ed. III Gozalo, R., ed. IV. García-Bellido, D., ed. 562 All rights reserved. No part of this publication may be reproduced or transmitted in any form or by any means, electronic or mechanical, including photocopy, recording, or any information storage and retrieval system now known or to be invented, without permission in writing from the publisher. References to this volume: It is suggested that either of the following alternatives should be used for future bibliographic references to the whole or part of this volume: Rábano, I., Gozalo, R. and García-Bellido, D. (eds.) 2008. Advances in trilobite research. Cuadernos del Museo Geominero, 9.
    [Show full text]
  • Adapazari Ovasi Ve Aşaği Sakarya Platosu'nda
    T.C. SAKARYA ÜN ĐVERS ĐTES Đ SOSYAL B ĐLĐMLER ENST ĐTÜSÜ ADAPAZARI OVASI VE A ŞAĞI SAKARYA PLATOSU’NDA TARIMSAL DE ĞĐŞĐ M YÜKSEK L ĐSANS TEZ Đ Kevser ZORLU Enstitü Anabilim Dal ı : Co ğrafya Tez Dan ış man ı: Yrd. Doç. Dr. Ali Y ĐĞĐ T HAZ ĐRAN - 2010 BEYAN Bu tezin yaz ılmas ında bilimsel yaz ım kurallar ına uyuldu ğunu, ba şkalar ının eserlerinden yararlan ılmas ı durumunda bilimsel normlara uygun olarak at ıfta bulunuldu ğunu, kullan ılan verilerde herhangi bir tahrifat yap ılmad ığı nı, tezin herhangi bir k ısm ının bu üniversite veya ba şka bir üniversitedeki ba şka bir tez çal ış mas ı olarak sunulmad ığı nı beyan ederim. Kevser ZORLU 30 / 05 / 2009 ÖNSÖZ “Adapazar ı Ovas ı ve A şağı Sakarya Platosun’nda Tar ımsal De ğişim” ad ını ta şı yan bu çal ış man ın konusunu Sakarya ilinde yeti ştirilen tar ım ürünlerinde geçmi şten günümüze ya şanan de ğişim ve nedenleri olu şturmaktad ır. Çal ış man ın giri ş bölümünde ara ştırma alan ının yeri, s ınırlar ı ve özellikleri; çal ış mada kullan ılan materyal, metot ve çal ış ma alan ıyla ilgili literatür özeti yer almaktad ır. Birinci bölümde Sakarya ilinde tar ımı etkileyen do ğal ve sosyo-ekonomik faktörler; ikinci bölümde ara ştırma alan ının tar ımsal yap ısı, özellikleri ve tar ımsal üretimde ya şanan de ğişim, nedenleri ile incelenmi ştir. Lisansüstü çal ış mamda dan ış manl ığı mı üstlenip, bu tezin konusunun belirlenmesinden, tamamlanmas ına kadar geçen sürede bana yard ımlar ı ve eme ği için Say ın Hocam Yrd.
    [Show full text]
  • Karabük İli Çevresel Durum Raporu
    Sayfa İÇİNDEKİLER No (A)KARABÜK İLİ ÇEVRESEL DURUM DEĞERLENDİRMESİ BÖLÜM I 2 COĞRAFİ KAPSAM 2 1.1 Karabük İli Coğrafi Durumu 3 1.2. Karabük İli Topoğrafyası 4 1.3. İklim 7 1.4. Ormanlar, Çayır ve Meralar 8 BÖLÜM II 9 SU/ATIKSU 9 2.1. SU KAYNAKLARI 9 2.1.1. İçme Suyu Kaynakları ve Barajlar 9 2.1.2. Yeraltı Su Kaynakları 9 2.1.3. Akarsular 9 2.1.4. Göller ve Göletler 10 2.2. SU KAYNAKLARININ KULLANIMI 11 2.3. SU KAYNAKLARININ DURUMU 12 2.3.1. İçme suyu kaynaklarında mevcut durum 12 2.3.2. Akarsularda Mevcut durum 27 2.4. ATIK SU SİSTEMİ, KANALİZASYON 30 2.5. KARABÜK İLİNDE SU KİRLİLİĞİNİN DEĞERLENDİRİLMESİ 37 BÖLÜM III 56 HAVA 56 3.1. ISINMADA KULLANILAN YAKITLAR 56 3.2.KARABÜK İLİ SANAYİ GRUPLANDIRILMASI 56 3.3. TRAFİKTEN KAYNAKLANAN EMİSYONLAR 64 3.4. HAVAYI KİRLETİCİ GAZLAR VE KAYNAKLARI 65 3.5.1. Partikül Madde (PM) ve SO2 Emisyonları 65 3.5. KARABÜK İLİNDE HAVA KİRLİLİĞİNİN DEĞERLENDİRİLMESİ 67 BÖLÜM IV 69 TOPRAK 69 4.1. KARABÜK İLİNDE PESTİSİT KULLANIMI 73 4.2 KARABÜK İLİNDE TOPRAK KİRLİLİĞİNİN DEĞERLENDİRİLMESİ 74 BÖLÜM V 78 ATIKLAR 78 5.1. KATI ATIKLAR 78 5.1.1. Ambalaj Atıkları 78 5.1.2. Tehlikeli Atıklar 81 5.1.3. Tıbbi Atıklar 82 5.1.4. Pil ve Aküler 83 5.1.5. Bitkisel Atık Yağlar 84 5.2 KATI ATIKLARIN DEPOLANMASI 84 5.3 KARABÜK İLİNDEKİ ATIK DURUMU VE DEĞERLENDİRİLMESİ 88 (B) BARTIN İLİ ÇEVRESEL DURUM DEĞERLENDİRMESİ BÖLÜM I 94 COĞRAFİ KAPSAM 94 1.1.
    [Show full text]
  • ZİRAİ İLAÇ BAYİLERİ 1 ADAPAZARI ÖZCAN TARIM 2 ADAPAZARI HUN TİCARET 3 ADAPAZARI Köseoğlu Süper Biofer 4 ADAPAZARI MOLÇOK TARIM 5 ADAPAZARI PANCAR EKİCİLERİ KOOP
    ZİRAİ İLAÇ BAYİLERİ 1 ADAPAZARI ÖZCAN TARIM 2 ADAPAZARI HUN TİCARET 3 ADAPAZARI Köseoğlu Süper Biofer 4 ADAPAZARI MOLÇOK TARIM 5 ADAPAZARI PANCAR EKİCİLERİ KOOP. 6 ADAPAZARI ÖZ BAHAR TARIM 7 ADAPAZARI 708 S. YAĞLI TOHUMLAR 8 ADAPAZARI SAKARYA TARIM MARKET 9 ADAPAZARI ZİRAAT ODASI-1 10 ADAPAZARI EYLÜL TARIM 11 ADAPAZARI ARYA Tarım 12 ADAPAZARI YALÇIN PAZARLAMA 13 ADAPAZARI PANCAR EKİCİLERİ KOOP. 14 ADAPAZARI SAKARYA TOHUM TAR.SAN. 15 ADAPAZARI May Ada Tarım(TOPTANCI) 16 ADAPAZARI Özcan Tarım 17 ADAPAZARI PANCAR EKİCİLERİ KOOP. 18 ADAPAZARI ÖNCÜ TOHUM 19 ADAPAZARI PİRİMOĞLU TARIM 20 ADAPAZARI BUDAKLAR T.K.K. 21 ADAPAZARI ADA TARIM 22 ADAPAZARI ÖZMEN TARIM 23 ADAPAZARI SALMANLI T.K.K. 24 ADAPAZARI KOÇ TARIM 25 ADAPAZARI ERN Tarım Ürünleri 26 ADAPAZARI Sakarya Rekor Tarım 27 AKYAZI S.S. APEK AKYAZI SATIŞ MAĞAZASI 28 AKYAZI SEÇKİN TARIM 29 AKYAZI S.S. APEK ÇATALKÖPRÜ SATIŞ MAĞAZASI 30 AKYAZI ARSLAN TARIM 31 AKYAZI SERA TARIM 32 AKYAZI 275 SAYILI AKYAZI TKK. 33 AKYAZI 2868 SAYILI OSMANBEY TKK. 34 AKYAZI 1680 SAYILI YENİORMANKÖY T.K.K 35 AKYAZI ENKA TARIM 36 ARİFİYE ÇETİN ELEKTRO PLASTİK A.Ş. 37 ARİFİYE 490 SAYILI ARİFİYE TKK. 38 ERENLER TEKNİK TARIM 39 ERENLER MODEL GÜBRE İLAÇ (TOPTANCI) 40 ERENLER S.S. APEK ERENLER SATIŞ MAĞAZASI 41 FERİZLİ ONUR TARIM 42 FERİZLİ 2720 SAYILI FERİZLİ TKK. 43 FERİZLİ 2842 SAYILI GÖLKENT TKK 44 FERİZLİ FERİZLİ ZİRAAT ODASI 45 FERİZLİ FERİZLİ TARIM OFİSİ 46 GEYVE YAVUZ TARIM 47 GEYVE 1097 SAYILI AKDOĞAN T.K.K. 48 GEYVE ÇİNİ TARIM 49 GEYVE GENÇLER TARIM 50 GEYVE S.S. APEK GEYVE SATIŞ MAĞAZASI 51 GEYVE 1090 SAYILI GEYVE T.K.K.
    [Show full text]
  • Sakarya Valiliği Çevre Ve Şehircilik Il Müdürlüğü
    T.C. SAKARYA VALİLİĞİ ÇEVRE VE ŞEHİRCİLİK İL MÜDÜRLÜĞÜ SAKARYA İLİ 2016 YILI ÇEVRE DURUM RAPORU HAZIRLAYAN: SAKARYA VALİLİĞİ ÇEVRE VE ŞEHİRCİLİK İL MÜDÜRLÜĞÜ SAKARYA-2017 i ÖNSÖZ Hızlı nüfus artıĢı neticesinde oluĢan çarpık kentleĢme, bu nüfusun ihtiyaçlarını karĢılayabilmek için yapılan plansız sanayileĢme ile kaynakların aĢırı ve kontrolsüz kullanımı sonucu oluĢan atık maddelerin miktarı ve çeĢidi artıĢ göstermiĢtir. Gerekli önlemler alınmadan kontrolsüz bir Ģekilde doğaya bırakılan atıkları doğanın kendi kendine bertaraf etmesi mümkün olmamakta ve sonucunda çevre kirliliği günümüzde artarak devam etmektedir. Bu durum hem canlıların sağlığını tehdit etmekte hem de ülkelerin maddi kaynaklarının ciddi bir miktarının çevre kirliliğinin giderilmesinde harcanmasına neden olmaktadır. Sağlıklı bir çevre ve yaĢam kalitesi yüksek bir toplum oluĢturmak, çevre sorunlarının çözülmesiyle mümkündür.Temiz çevreye sahip, atık yönetim sistemlerini kuran Ģehirler modern ve yaĢanılabilir Ģehirler olarak kabul edilmektedir. Çevre kirliliği konusunda alınması gereken teknik ve ekonomik önlemlerin yanında öncelikle toplumda çevre bilincinin oluĢturulması gerekmektedir. Ġnsanlarımızı küçük yaĢlardan baĢlayarak çevre konusunda eğitmek durumundayız. Unutulmamalıdır ki çevreyi kirletmemek, kirlendikten sonra temizlemekten çok daha kolay ve ekonomiktir. Gelecek nesillere yaĢanabilir temiz bir çevre bırakabilmek için duyarlı davranmak hepimize düĢen önemli bir insanlık görevidir. Hazırlanan Çevre Durum Raporunun; çevrenin korunmasında, hava, toprak, su ve gürültü
    [Show full text]
  • Urban Identity and Tourism Impact Assesment
    THE IMPACT OF ECONOMIC AND SOCIAL DEVELOPMENT IN SAFRANBOLU A THESIS SUBMITTED TO THE GRADUATE SCHOOL OF NATURAL AND APPLIED SCIENCES OF THE MIDDLE EAST TECHNICAL UNIVERSITY BY SĠBEL AKPINAR KASAP IN PARTIAL FULFILLMENT OF THE REQUIREMENTS FOR THE DEGREE OF DOCTOR OF CITY AND REGIONAL PLANNING IN THE DEPARTMENT OF CITY AND REGIONAL PLANNING JANUARY 2011 Approval of the thesis: THE IMPACT OF ECONOMIC AND SOCIAL DEVELOPMENT IN SAFRANBOLU submitted by Sibel AKPINAR KASAP in partial fulfillment of the requirements for the degree of Doctor of City and Regional Planning in City and Regional Planning Department, Middle East Technical University by, Prof. Dr. Canan ÖZGEN _____________________ Dean, Graduate School of Natural and Applied Sciences Prof. Dr. Melih ERSOY _____________________ Head of Department, City and Regional Planning Assoc. Prof. Dr. Gülden BERKMAN _____________________ Supervisor, City and Regional Planning Dept., METU Assoc. Prof. Dr. C. Nil UZUN _____________________ Co-Supervisor, City and Regional Planning Dept., METU Examining Committee Members: Assoc. Prof. Dr. Serap KAYASÜ _____________________ City and Regional Planning Dept., METU Assoc. Prof. Dr. Gülden BERKMAN _____________________ City and Regional Planning Dept., METU Assoc. Prof. Dr. H. Tarık ġENGÜL _____________________ Political Science and Public Administration Dept., METU Assoc. Prof. Dr. Ela BABALIK SUTCLIFFE _____________________ City and Regional Planning Dept., METU Assist. Prof. Dr. Ġsmail TANER _____________________ City and Regional Planning Dept., Abant Izzet Baysal Uni. Date: 27.01.2011 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.
    [Show full text]
  • An Example of Tick-Crimean Congo Hemorrhagic Fever (CCHF) in Eflani District, Karabuk, Turkey
    Scientific Research and Essays Vol. 6(11), pp. 2395-2402, 4 June, 2011 Available online at http://www.academicjournals.org/SRE DOI: 10.5897/SRE11.574 ISSN 1992-2248 ©2011 Academic Journals Full Length Research Paper An example of tick-Crimean Congo hemorrhagic fever (CCHF) in Eflani district, Karabuk, Turkey Guzin Kanturk Yigit Department of Geography, Faculty of Literature, Karabuk University, 78050 Karabuk, Turkey. E-mail: [email protected]. Accepted 6 May, 2011 Ticks are the ectoparasites that threatening animal and human health. Their effects on human health have started to attract attention, especially after the 1980s. Ticks can be seen in many parts of the world. Ticks are active during certain periods; many tick species are active between spring and autumn months. Tick bites may not be noticed immediately; when it is noticed, it should be immediately removed. While the tick is being removed, it is necessary to comply with certain rules. In this study, tick cases in the world and Turkey were mentioned then numbers of tick cases in Karabuk were investigated. The aim of the study is to examine the number of recorded cases in Eflani (Karabuk). The aim of the study is to examine the number of recorded cases in Eflani. The case records of Karabuk provincial health directorate about Crimean Congo hemorrhagic fever (CCHF) were used in the research. At the end of the study, it was concluded that Eflani is the district that has more tick cases in the Province of Karabuk with its suitable geographical conditions to host ticks. Key words: Tick, Crimean Congo hemorrhagic fever (CCHF), Eflani, Karabuk, Turkey.
    [Show full text]
  • T.C. Sakarya Valiliği
    T.C. SAKARYA VALİLİĞİ MAYIS-2015 İÇİNDEKİLER GİRİŞ... ...................................................................................................................... …3 İL HAKKINDA SAYISAL BİLGİLER... ...................................................................... …5 SOSYAL DURUM... .................................................................................................. …9 1) NÜFUS ve YÖNETİM DURUMU ........................................................................... 9 2) EĞİTİM DURUMU. ....................................................................................... ……11 3) SAĞLIK ................................................................................................................ 18 4) KÜLTÜR ve TURİZM ........................................................................................... 22 5) GENÇLİK HİZMETLERİ ve SPOR ................................................................... … 29 6) MALİYE ............................................................................................................... 33 7) AİLE ve SOSYAL POLİTİKALAR ...................................................................... .. 35 8) SOSYAL YARDIMLAŞMA ve DAYANIŞMA VAKIFLARI ..................................... 38 9) SOSYAL GÜVENLİK ........................................................................................... 41 10) TAPU ve KADASTRO DURUMU ....................................................................... 42 EKONOMİ .................................................................................................................
    [Show full text]