DOCSLIB.ORG

Autochthonous Upper Permian (Midian) Carbonates In

Total Page：16

File Type：pdf, Size：1020Kb

Download full-text PDF Read full-text
Autochthonous Upper Permian (Midian) Carbonates In TurkishJournalofEarthSciences (TurkishJ.EarthSci.),Vol.13, 2004,pp.215-229. Copyright©TÜB‹TAK AutochthonousUpperPermian(Midian)Carbonates intheWesternSakaryaCompositeTerrane,GeyveArea, Turkey:PreliminaryData NECAT‹TURHAN1,CENG‹ZOKUYUCU1 &M.CEMALGÖNCÜO⁄LU2 1 DepartmentofGeologicalResearch,GeneralDirectorateofMineralResearchandExploration(MTA), TR-06520Ankara,Turkey 2 DepartmentofGeologicalEngineering,MiddleEastTechnicalUniversity, TR-06531Ankara,Turkey(e-mail:[email protected]) Abstract: Permianlimestonesoccurwidelywithintheclasticunitsofthe“KarakayaComplex”andareinterpreted asallochthonousbodiesorolistoliths.IntheKadirlerareatothesouthofGeyve,however,UpperPermian(Midian) quartzsandstonesandcarbonateswitharichforaminiferfaunadisconformablyoverlieacrystallinebasement complex.Thisbasementcomplexcomprisesmetaclasticrocks,recrystallisedlimestones,metacherts,and metadiabases,andisintrudedbygranodiorites.Theoverlyingbasalconglomeratesandquartziticsandstonesare dominatedbypebblesfromthebasementcomplexandarefollowedupwardbymedium-tothick-bedded dolomites,dolomiticlimestonesandlimestones. TheforaminiferalassemblagewithNeoschwagerinahaydeni DutkevitchandKhabakov,Neoschwagerina ex.gr. ventricosa Skinner, Charliellarossae Alt›nerandÖzkan-Alt›ner, Hemigordiopsisrenzi Reichel, Yabeina sp., Pseudokahlerina sp.andKahlerina sp.inthesecarbonatesisindicativeofdepositioninashelf-lagoonduringthe MidianstageoftheLatePermian. ThisnewfindingconstitutesfurthersupportformodelsthatsuggestacompositecharacterfortheSakarya Terrane,andthatthe“Karakayabasin”inNWAnatoliaopenedaboveaVariscan-consolidatedcrustalbasementand itsPermianplatform,whencethelimestoneolistolithsofthe“KarakayaComplex”weremainlyderived.Moreover, theMidiantransgressionandtheforaminiferalassemblageinthestudiedsuccessionsaretypicalfeaturesofthe northernTauride-AnatolidePlatform,indicatingthattheSakaryaCompositeTerranewasattachedtothelatter priortotheopeningofthe‹zmir-AnkarabranchofNeotethys. KeyWords: KarakayaComplex,basement,autochthon,limestone,UpperPermian SakaryaKompozitBirli¤iBat›s›nda(Geyve,Türkiye)OtoktonÜstPermiyen (Midiyen)Karbonatlar›:ÖnBulgular Özet: Permiyenyafll›kireçtafllar›“KarakayaKompleksi”nink›r›nt›l›birimleriiçindeyayg›nolarakgözlenirlerve alloktonkütlelerveyaolistolitlerolarakyorumlan›rlar.Ancak,Geyve’ningüneyinde,Kadirleryöresinde foraminifercezenginkumtafllar›vekireçtafllar›metamorfikbirtemelüzerindeuyumsuzolarakyeralmaktad›r. Metamorfiktemel;metak›r›nt›l›kayalar,rekristalizekireçtafllar›,metaçörtlervemetadiyabazlardanoluflurvebir granodiyoritkütlesitaraf›ndankesilmifltir.Butemelüzerindeyeralantabankonglomeras›vekuvarsitikkumtafllar› metamorfiktemeldentüremeçak›llariçerirveüstedo¤ruorta-kal›ntabakal›dolomitler,dolomitikkireçtafllar›ve kireçtafllar›nageçifllidir. Karbonatkayalar›n›nkapsad›¤›foraminifertoplulu¤u( Neoschwagerinahaydeni DutkevitchandKhabakov, Neoschwagerina ex.gr. ventricosa Skinner, Charliellarossae Alt›nerandÖzkan-Alt›ner, Hemigordiopsisrenzi Reichel,Yabeina sp.,Pseudokahlerina sp.ve Kahlerina sp.),bubiriminMidiyens›ras›ndas›¤denizelbirortamda (flelflagünü)çökeldi¤inigösterir. Bubulgu,“SakaryaTektonikBirli¤inin”kompozitnitelikteoldu¤u,Karakayabaseni'ninPermiyenplatform karbonatlar›ileörtülübirVariskenk›tasalkabukparças›üzerindeaç›ld›¤›veiçindeyeralankireçtafl›olistolitlerinin buplatformdankaynakland›¤›hususundakigörüflleridesteklemektedir.‹ncelenenalandakibelirginMidiyen transgresyonuveforaminifertoplulu¤uToroslar›nkuzeykesimiileözdeflnitelikteolup,SakaryaveTorid-Anatolid tektonikbirliklerininNeotetis’in‹zmir-Ankarakoluaç›lanade¤inbitiflikolduklar›naiflaretetmektedir. AnahtarSözcükler:KarakayaKompleksi,otokton,temel,kireçtafl›,ÜstPermiyen 215 AUTOCHTHONOUSMIDIANCARBONATESINTHEWESTERNSAKARYACOMPOSITETERRANE Introduction Mesozoicage”.Withsomedifferencesinthetimingofthe Oneofthemostdebatedissuesconcerningthegeology events,fiengör etal. (1984),Göncüo¤lu etal. (1987), ofNWTurkeyisthegeologicalevolutionoftheKarakaya Okayetal. (1991)and,Y›lmaz etal. (1995)havenoted ComplexinNWAnatolia.Theterm“Karakaya”was thatthebasementrocksarecharacterisedbyaVariscan- initiallyintroducedbyBingöl(1968)asthe“Karakaya consolidatedcrystallinecomplex(Sakaryabasement)and Series”,foraslightlymetamorphicsuccessionat itsUpperPalaeozoiccarbonatecover.Thelatter KarakayaHilltothesouthofBeyobas›Villageinthe representsthenorthernmarginoftheGondwanan Edremitarea,NWAnatolia.Sincethen,thenamehas Tauride-Anatolideunit,uponwhichtheTriassicKarakaya beenappliedbydifferentauthorstoawiderangeof clasticrocksformedinamarginalbasin,abovethe rockunitsindifferentpartsofnorthwesternand southward-subductingPalaeotethyanoceaniclithosphere northernAnatolia(Figure1a).Tekeli(1981)proposed (Figure2a).Okayetal. (1996)andLeven&Okay(1996) thatthispartlymetamorphicandextremelytectonised proposedacompletelydifferentscenario,inwhichthe assemblagerepresentstheremnantsoftheLate SakaryabasementwasattachedtotheLaurasianmargin Palaeozoic–EarlyMesozoicPalaeotethysoffiengör nexttothe‹stanbulUnit.AlltheTriassicKarakayaunits (1979)(forabriefreviewseeOkayetal. 1996;Okay& (Nilüfer:Early–MiddleTriassicfore-arc,Çal:islandarcor Göncüo¤lu2002). matureseamountwithPermo–Triassiccarbonate platform,HodulandOrhanlar:Middle–LateTriassic Thecontroversyregardingtheoverallgeodynamic accretionarycomplexes,Denizgören:Triassicophiolites) evolutionalsoincludesthecrystalline“basementrocks”of wereformedduringtheclosureofthePalaeotethys.The theKarakayaComplex,theirpalaeogeographiclocation, Permiancarbonates(includingtheEzineUnit)were ageandcontactrelationswiththePermo–Triassicnon- derivedfromaTauride-Anatolide-typecontinentalsliver, to-slightlymetamorphicsedimentaryandvolcanicrocks. whichwasriftedfromthelatterbyback-arcspreading Tekeli(1981)’soriginalsuggestionwasthatthe (Figure2b)resultingintheopeningofthe‹zmir-Ankara “metamorphicsatthebase”were“coevalwiththe branchofNeotethys. Karakayamélangeand,hence,ofLate Palaeozoic–Early A BLACK SEA N B N Bahaiye ÝSTANBUL (Esenköy) EXPLANATIONS ANKARA Muttalip Göçük D. post-Triassic cover Study Area (Figure 1b) ÝZMÝR 0 100 km Sakarya Composite Terrane Pazarkaya T. Karaoluk T. recrystallized limestone and Alýplar Karþýköy pillow basalts Koca D. Asarkaya T. arkosic sandstones Triassic Yukarýyayla U. Permian- Derbent Limestone Çinetaþý T. Canbazkaya Formation Figure 3a U. Permian Sindir D. granodiorite Cumalý black recrystallized limestones 0 500 1000 m Kayýplar Figure 3b Kabaklý D. (Aragat) Kadirler pre-Permian micaschists, metacherts, metarhyolites (undifferentiated) normal reverse contact foliation bedding a fault fault Figure1. (a)DistributionoftheSakaryaCompositeTerraneinNWAnatoliaand (b) thegeologicalmapofthestudyareawithandthelocationsof thestudiedsections. 216 N.TURHANET AL. a Early Triassic b L. Permian te Moesia li Ýstanbul Zone i o h p V Stranja o V Sakarya Zone V Zone n e V Karakaya r ö Rift g V (future Neotethyan z i n V Vardar ocean) V PALEO-TETHYS De V Volcanic arc V V V V Unit V V Nilüfer V back-arc rifting K V IDE BLOC V Ýzmir-Ankara Rift AUR Pindos V - T IDE TOL Okay et al. 1991 ANA Okay et al. 1996 c NS Late Permian EURASIA subduction GONDWANA jamming Çanðaldað arc or equivalent carbonate platforms on Gondwanan continental slivers MODEL 1 site of new subduction zone MODEL 2 Karakaya Complex Karakaya Complex Early Triasic ophiolite formation ophiolite formation rifting (i.e., Chios, Karaburun) Pickett & Robertson 1996 d Tauride-Anatolide Platform Late Permian Future Sakarya Microcontinent deposition of the platform carbonates Paleotethys Hercynian consolidated basement opening of Karakaya Early Triassic Basin s.s. deposition of continental clastics closure of Paleotethys rifting along KBB uplift Göncüoðlu et al. 2000a e South North SOUTHERN BIOFACIES NORTHERN BIOFACIES BELT BELT BEYÞEHÝR - AKSEKÝ - HADIM HIGH DEPOSITIONAL BASEMENT OF FUTURE AREA OF SAKARYA CONTINENT ANTALYA or GEYÝK DAÐI ALADAÐ BOLKAR DAÐI UPPER PERMIAN ALANYA ? BLOCKS OF (Hercynian Orogen) KARAKAYA UNITS Permian ? PRE- ? LATE PERMIAN ? ? ? Altýner et al. 2000 ORDOVICIAN DEVONIAN CARBONIFEROUS LOWER PERMIAN UPPER PERMIAN f Çal Unit SNOrhanlar Greywacke Nilüfer oceanic plateau Laurasian margin (a) Mid Triassic Okay 2000 Figure2. CartoonsofpreviouslysuggestedgeodynamicmodelsfortheevolutionoftheKarakaya units.Forthedetailsconcerningthecartoons,seetext. 217 AUTOCHTHONOUSMIDIANCARBONATESINTHEWESTERNSAKARYACOMPOSITETERRANE Pickett&Robertson(1996)’smodelinvolvesthe underlainthePermo–Carboniferouslimestonesinthe closureofthePalaeotethysbysouthandnorthward SakaryaZone”asclearlyformulatedbyOkay(2000). subduction(Figure2c).TheyconsideredtheKarakaya Inthisstudy,wewillfirstbrieflysummarisethe ComplexasaPalaeotethyanaccretionarycomplexwith previousdataonthebasementrocksoftheKarakayaunit Triassicophiolites(DenizgörenOphiolite),seamounts andtheirrelationswithPermianlimestones.Fieldand (NilüferUnit),trenchsequences(OrtaobaUnit)abyssal- palaeontologicaldatafromtheGeyveareawillthenbe plaindeposits(KalabakUnit)andPermiancarbonate presentedandtheevolutionofthe“KarakayaComplex” platformsonGondwanancontinentalsliverswithintra- discussed. platformrifts(ÇalUnit). Göncüo¤luetal. (1997,2000c)pointedoutthatthe pre-Liassic“KarakayaComplex”withintheAlpineSakarya ReviewofPreviousInterpretations unitinnorthernTurkeyactuallyincludesremnantsof AccordingtotheoriginaldescriptionofBingöl(1968), Variscanbasement,aTriassicrift-complexformedabove theKarakayaunitincludesinitstypelocalityquartzites, itsPermiancover,aswellasthrustslicesofthe feldspathicsandstone,metaspiliteandmetamorphosed Palaeotethyanorogeniccomplex(Figure2d).Itwasalso spiliticbasaltsthatdisconformablyoverliethecrystalline
Load more

Recommended publications
  • Kurum Kodu İlçesi Kurum Adı Münhal Norm 1 731957
    Kurum Münhal İlçesi Kurum Adı Kodu Norm 1 731957 ADAPAZARI 17 Ağustos İlkokulu 1 2 731963 ADAPAZARI 21 Haziran İlkokulu 1 3 733115 ADAPAZARI Adapazarı İmam Hatip Ortaokulu 1 4 270899 ADAPAZARI Adapazarı Mesleki Eğitim Merkezi 1 5 194100 ADAPAZARI Adapazarı Mesleki ve Teknik Anadolu Lisesi 1 6 747014 ADAPAZARI Adapazarı Özel Eğitim Anaokulu 1 7 194112 ADAPAZARI Adapazarı Prof. Dr.Tansu Çiller Mesleki ve Teknik Anadolu Lisesi 1 8 732138 ADAPAZARI Atatürk İlkokulu 1 9 732141 ADAPAZARI Aykut Yiğit Ortaokulu 1 10 732888 ADAPAZARI Bayraktar İlkokulu 1 11 732143 ADAPAZARI Berna Yılmaz İlkokulu 1 12 732147 ADAPAZARI Budaklar İlkokulu 1 13 732156 ADAPAZARI Evrenköy İlkokulu 1 14 732158 ADAPAZARI Fatih İlkokulu 1 15 966759 ADAPAZARI Fatmana Okutan Anaokulu 1 16 964614 ADAPAZARI İMKB Mehmet Akif Ersoy Mesleki ve Teknik Anadolu Lisesi 1 17 194089 ADAPAZARI İMKB Sakarya Mesleki ve Teknik Anadolu Lisesi 1 18 732177 ADAPAZARI İstiklal Ortaokulu 1 19 732163 ADAPAZARI Karadere İlkokulu 1 20 732165 ADAPAZARI Karakamış İlkokulu 1 21 764413 ADAPAZARI Korucuk Anaokulu 1 22 732171 ADAPAZARI Köprübaşı İlkokulu 1 23 732175 ADAPAZARI Kurtuluş Ortaokulu 1 24 761579 ADAPAZARI Medine Müdafii Fahreddin Paşa İmam Hatip Ortaokulu 1 25 732178 ADAPAZARI Mehmet Nuri İlkokulu 1 26 751968 ADAPAZARI Mevlana İmam Hatip Ortaokulu 1 27 732238 ADAPAZARI Mithatpaşa Ortaokulu 1 28 732182 ADAPAZARI Murtaza Erdoğan İlkokulu 1 29 732205 ADAPAZARI Namık Kemal Ortaokulu 1 30 732255 ADAPAZARI Ozanlar Ortaokulu 1 31 732221 ADAPAZARI Sabihahanım Ortaokulu 1 32 732226 ADAPAZARI Sakarya
    [Show full text]
  • Segment Structure of the Southern Strand of the North Anatolian Fault System and Paleoseismic Behaviour of the Gemlik Fault, NW Anatolia
    Segment Structure of the Southern Strand of the North Anatolian Fault System and Paleoseismic Behaviour of the Gemlik Fault, NW Anatolia Selim Özalp, Ömer Emre and Ahmet Doğan General Directorate of Mineral Research and Exploration (MTA), Department of Geological Research 06520, Ankara, Turkey The North Anatolian Fault System (NAFS) is a transform fault that accommodates relative motion between Anatolian and Black Sea microplates. The NAFS bifurcates two strands as the Northern and the Southern in the Marmara region. Recent lateral motion is about 24 mm/yr along the NAFS. According to the recent GPS data, there is a slip partitioning between both strands and the northern strand carries approximately 3 times as much right-lateral motion as does the southern strand. Therefore we interpret that the northern strand is the master zone which accommodate majority of the recent lateral motion. In this study, the southern strand is extending between Dokurcun valley and Bandırma bay is evaluated as a splay instead of a main strand diverging from the NAFS as described in previous studies. This splay is included in NW Anatolia transition zone which characterizes bend structures. Length of the southern strand is about 140 km between Dokurcun valley and Gemlik bay along Pamukova basin, Lake İznik and Gemlik Bay depressions. The strand can be divided into three main geometric segments in right steeping pattern. Those are Geyve, İznik and Gemlik, from east to west. Length of the Geyve Fault is about 57 km and general trend is N70°E. The İznik Fault is about 56 km-long trending of N75°E.
    [Show full text]
  • The Representation of Ethnic Minorities in Twentieth Century Turkish Fiction
    The Representation of Ethnic Minorities in Twentieth Century Turkish Fiction Ruth Margaret Whitehouse School of Oriental and African Studies London University ProQuest Number: 10672680 All rights reserved INFORMATION TO ALL USERS The quality of this reproduction is dependent upon the quality of the copy submitted. In the unlikely event that the author did not send a com plete manuscript and there are missing pages, these will be noted. Also, if material had to be removed, a note will indicate the deletion. uest ProQuest 10672680 Published by ProQuest LLC(2017). Copyright of the Dissertation is held by the Author. All rights reserved. This work is protected against unauthorized copying under Title 17, United States C ode Microform Edition © ProQuest LLC. ProQuest LLC. 789 East Eisenhower Parkway P.O. Box 1346 Ann Arbor, Ml 48106- 1346 Abstract During the first half of the twentieth century, the ethnically segmented Ottoman empire was transformed into a nation state of Turkish citizens. This thesis explores and evaluates the representation of ethnic minorities in Turkish fiction against a background of demographic, political, and social change. Within this context, novels and short stories of selected writers have been studied with a view to determining differences of experience, perception and attitude. The writers include: Huseyin Rahmi Giirpmar, Halide Edip Adivar, Re§at Nuri Guntekin, Halikarnas Bahk9isi, Orhan Kemal, Haldun Taner, Sait Faik, and Ya§ar Kemal. The thesis comprises an introduction, three chapters and a conclusion. The Introduction gives a brief overview of historical events relating to demographic changes and ethnic minority status, and looks at the popular perception of minorities in the Ottoman performance arts.
    [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]
  • The Bryophyte Flora of Akyazı, Arifiye, Geyve, Karapürçek Districts (Sakarya, Turkey)
    www.biodicon.com Biological Diversity and Conservation ISSN 1308-8084 Online ISSN 1308-5301 Print Research article/Araştırma makalesi 13/1 (2020) 27-43 DOI: 10.46309/biodicon.2020.731878 The bryophyte flora of Akyazı, Arifiye, Geyve, Karapürçek districts (Sakarya, Turkey) Güray UYAR *1, Muhammet ÖREN2 & Mevlüt ALATAŞ3 ORCID: 0000-0003-4038-6107; 0000-0003-1839-3087; 0000-0003-0862-0258 1 Ankara Hacı Bayram Veli University, Polatlı Faculty of Science & Arts, Depart. of Biology, 06900, Ankara, Turkey 2 Zonguldak Bülent Ecevit University, Faculty of Science & Arts, Department of Biology, 67100, Zonguldak, Turkey 3 Munzur University, Faculty of Engineering, Department of Bioengineering, 62000, Tunceli, Turkey Abstract In this study, bryophyte flora of the Akyazı, Arifiye, Geyve, Karapürçek districts in Sakarya Province of Turkey was found out. A total of 1037 bryophyte specimens were collected from the research area in the different vegetation periods between 2016 and 2017. As a results of this study; 193 taxa (1 hornwort, 34 liverworts, 158 mosses) belonging to 113 genera and 55 families were determined. Among them, Sphagnum contortum Schultz is recorded for the second time from Turkey and also 11 taxa are new for the A2 grid-square according to the Turkish grid square system adopted by Henderson (1961). In addition, in the floristic list all taxa, with their Turkey distributions, which are determined by reviewing the related all literatures, and IUCN categories in European countries, moreover life forms of bryophytes and some ecological features such as; (humidity, light, acidity) are given. Key words: bryophyte, flora, Akyazı, Arifiye, Geyve, Karapürçek ---------- ---------- Akyazı, Arifiye, Geyve, Karapürçek ilçeleri (Sakarya, Turkey) briyofit florası Özet Bu çalışmada, Türkiye’nin Sakarya iline bağlı Akyazı, Arifiye, Geyve, Karapürçek ilçelerinin briyofit florası ortaya çıkartılmıştır.
    [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]
  • Invest in Bilecik
    www.bebka.org.tr • www.investinbilecik.gov.tr SPECIAL INVESTMENT ZONES ORGANISED INDUSTRY ZONES (OIZ) OF BİLECİK WHY BİLECİK? • 6 Organised Industry Zones + ongoing new ones OIZ Status Type • Bozüyük Gündüzbey Logistics Centre: It's under the construction and located next to Bozuyuk OIZ where will 1 Bilecik 1. OIZ Active Mixed have railway connection as well.It is located next to A suitable investment environment 4th Regional Incentive Advantages with a total of 6 organized industrial Bozüyük OIZ and will have railway connection. 200,000 2 Bilecik 2. OIZ Active Mixed for Investments in OIZs people are expected to be employed in the centre when it's zones and the new one under construction INVEST IN completed. 3 Bozüyük OIZ Active Mixed Active Mixed 4 Osmaneli OIZ Close to domestic and international Fast train connection between Söğüt OIZ Active Mixed markets with strategic geographical Istanbul - Ankara - Konya makes Osmaneli 5 location easy and convenient transportation BiLECiK Gölpazarı 6 Pazaryeri OIZ Active Mixed Yenipazar Bilecik 7 Bilecik 3.OIZ Ongoing Mixed BİLECİK Land, rail and marine networks that Growing R&D and clustering Söğüt İnhisar Pazaryeri providing logistical links network in ceramic industry TURKEY Bozüyük NUMBER OF NUMBER MOBILE PHONE INTERNATIONAL OF BROADBAND Natural stone sources (famous Rich agricultural product quality SUBSCRIPTIONS SUBSCRIPTIONS Bilecik Beige marble) and diversity LOGISTICS Ankara İstanbul Bursa-Gemlik Port 178,236 171,169 Distance (km) 315 247 97 Bursa Eskişehir Bilecik Development Agency (BEBKA) The best quality hops plant in the Developing university and skilled world is cultivated in the district of Bilecik Investment Support Office workforce potential Bilecik 1.
    [Show full text]
  • Rozwój Kolei Dużych Prędkości W Warunkach Krajów Rozwijających Się – Przypadek Turcji
    Systemy transportowe Elektryczny zespół trakcyjny serii 80000 na stacji w Ankarze (11.05.2018) Andrzej Massel Rozwój kolei dużych prędkości w warunkach krajów rozwijających się – przypadek Turcji System kolei dużych prędkości w Turcji należy do najszybciej roz- przeanalizowano czynniki społeczne i gospodarcze, które umoż- wijających się na świecie. Pierwszy odcinek Ankara–Eskişehir liwiły jego powstanie. został uruchomiony w 2009 roku. Tymczasem, według danych UIC z 1 kwietnia 2018 roku, długość eksploatowanych linii dużych Rozwój transportu kolejowego w Turcji prędkości osiągnęła już 724 km. Ponadto 1 395 km takich linii Historia kolei na terenie Turcji rozpoczęła się wraz z wydaniem znajduje się w budowie, a następne 1 127 km jest w fazie pla- przywileju budowy linii Izmir–Aydin w dniu 23 września 1856 nowania [9]. Władze państwowe postawiły cel, aby w 2023 roku, roku [3]. Budowa tej linii, o długości 130 km, została ukończona czyli w 100-lecie istnienia Republiki, koleje dużych prędkości ob- w 1866 roku. Niemal równocześnie z nią powstały także inne sługiwały połowę ludności i 18 z 81 prowincji kraju [23]. Symbo- linie w rejonie Izmiru, w tym linia Izmir–Kasaba (Turgutlu), sta- liczne znaczenie miał fakt, że 10 Światowy Kongres Kolei Dużych nowiąca pierwszą część połączenia do Afyon, a także odcinek Prędkości UIC odbył się właśnie w stolicy Turcji, Ankarze, w dniach linii Manisa–Bandirma o długości 98 km (pozostała część tej 8-11 maja 2018 roku. linii powstała w latach późniejszych). W latach 1871-1873 powstała tak zwana „Kolej Rumelijska” Stambuł–Edirne (Adrianopol), która z czasem stała się głównym W artykule omówiono genezę i charakterystyczne cechy kolei połączeniem stolicy Imperium z Europą.
    [Show full text]
  • Cydonia Oblonga MILL.) Gardens by Leaf Analysis in Geyve District, Sakarya
    MAS Journal of Applied Sciences 6(2): 312–324, 2021 DOI: http://dx.doi.org/10.52520/masjaps.34 Araştırma Makalesi Determination of Nutrition Status of Quince (Cydonia oblonga MILL.) Gardens By Leaf Analysis in Geyve District, Sakarya Ahmet Çağlar MUMCUOĞLU1, Korkmaz BELLİTÜRK2* 1T.C. Ministry of Agriculture and Forestry, Istanbul Provincial Directorate of Agriculture and Forestry, İstanbul 2Tekirdağ Namık Kemal University Faculty of Agriculture, Department of Soil Science and Plant Nutrition, Tekirdağ *Corresponding author: [email protected] Geliş Tarihi: 17.02.2021 Kabul Tarihi: 25.03.2021 Abstract This research was carried out in order to determine the nutritional status of quince gardens in villages where Eşme variety quince (Cydonia oblonga Mill.) Is grown in Sakarya province, Geyve district. Nitrogen (N), phosphorus (P), potassium (K), calcium (Ca), magnesium (Mg), iron in leaf samples taken from 34 quince gardens in 13 villages where Eşme variety is intensively cultivated, 8-12 weeks after the full flowering period. (Fe), Copper (Cu), zinc (Zn) and manganese (Mn) concentrations were determined. Since there are no limit values determined for evaluating the results of herbal analysis related to quince in the literature, the values determined for pear (Pyrus communis) and apple (Malus domestica), which are from the same family with the quince (Rosaceae), were taken as reference. The reason for using the reference values determined for pear in the literature; It is the use of quince rootstocks for dwarfing the pear plant. N 9% deficiency, 91% sufficient in leaf samples taken from quince gardens in the research area; P 100% is sufficient; K 6% deficient, 85% sufficient, 9% high; Ca 18% sufficient, 82% high; Mg 69% sufficient, 31% high; Fe 97% sufficient, 3% high; Mn 23% deficient, 74% adequate, 3% high; Zn 50% deficient, 47% sufficient, 3% high; Plant nutrient levels were determined as 100% higher than Cu.
    [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]
  • Second Millennium Site Distribution and Pottery of Inland Northwestern Anatolia
    Anatolia Antiqua Revue internationale d'archéologie anatolienne XXIV | 2016 Varia Second Millennium Site Distribution and Pottery of Inland Northwestern Anatolia Turan Efe and Bérengère Perello Electronic version URL: http://journals.openedition.org/anatoliaantiqua/371 DOI: 10.4000/anatoliaantiqua.371 Publisher IFEA Printed version Date of publication: 1 May 2016 Number of pages: 35-89 ISBN: 9782362450648 ISSN: 1018-1946 Electronic reference Turan Efe and Bérengère Perello, “Second Millennium Site Distribution and Pottery of Inland Northwestern Anatolia”, Anatolia Antiqua [Online], XXIV | 2016, Online since 11 December 2018, connection on 16 February 2021. URL: http://journals.openedition.org/anatoliaantiqua/371 ; DOI: https://doi.org/10.4000/anatoliaantiqua.371 Anatolia Antiqua TABLE DES MATIERES Ergul KODAS, Le surmodelage du crâne au Néolithique au Proche-Orient : techniques de surmodelage et expérimentations 1 Isabella CANEVA et Eric JEAN, Mersin-Yumuktepe : une mise au point sur les derniers travaux 13 Turan EFE et Bérengère PERELLO, Second Millenium site distribution and pottery of Inland Northwestern Anatolia 35 Antoine PEREZ, Amida 6 : Antiochos IV, le ‟Hanigalbat” et la Sophène 91 Ergün LAFLI et Hadrien BRU, Inscriptions et monuments funéraires gréco-romains d’Anatolie occidentale 103 Oğuz TEKİN et Aliye EROL-ÖZDİZBAY, Coins from Allianoi excavations: Campaign of 2001 117 Nuran ŞAHİN, Etude iconographique des monnaies autonomes frappées par Colophon-sur-Mer : nouveaux acquis 147 Vera SAUER, Konventionelle Individualität. Zur
    [Show full text]
  • GELİŞİMİ VE DAĞILIŞI AÇISINDAN OSMANELİ İLÇESİNDESANAYİ FAALİYETLERİNİN İNCELENMESİ1 Zafer BAŞKAYA Özet
    Zafer BAŞKAYA / 16 GELİŞİMİ VE DAĞILIŞI AÇISINDAN OSMANELİ İLÇESİNDESANAYİ FAALİYETLERİNİN 1 İNCELENMESİ Zafer BAŞKAYA Özet Marmara Bölgesi’nin Güney Marmara Bölümü’nde yer alan Osmaneli ilçesi, idari açıdan Bilecik iline bağlıdır. Kuzeyden İznik (Bursa) ve Pamukova (Sakarya), doğudan Geyve (Sakarya) ve Gölpazarı (Bilecik), güneyden Bilecik Merkez, batıda Yenişehir (Bursa) ve İznik (Bursa) ilçeleri ile komşudur. 1970’li yıllara kadar sanayi faaliyetleri bakımından gelişmemiş olan Bilecik ili 1973 yılında 3. Beş Yıllık Kalkınma Planı’nda kalkınmada öncelikli iller kapsamına alınmıştır. Bu süreçle beraber daha sonraki yıllarda Osmaneli ilçesinin de yer aldığı il genelinde sanayi tesislerinin sayısında hızlı bir artış yaşanmıştır. Osmaneli ilçesi de bu durumdan olumlu etkilenmiştir. Buna ek olarak, ilçenin konum itibariyle pazar şartları açısından İstanbul, İzmit, Adapazarı, Bursa ve Eskişehir gibi önemli şehirlere yakın olması ve Bilecik-İstanbul karayolu güzergahı üzerinde yer alması sanayi faaliyetleri açısından önemini daha da artırmıştır. Yöredeki sanayi tesislerinde kullanılan hammaddenin önemli bir kısmının yakın çevreden sağlanması nedeniyle ilçedeki sanayi faaliyetleri anayolların kavşak noktasında bulunan Osmaneli ilçe merkezi ve çevresinde yoğunlaşmıştır. Dolayısıyla bu çalışmada Osmaneli ilçesinin sanayi faaliyetlerinde etkili olan faktörler ile sanayi faaliyetlerinde geçmişten günümüze meydana gelen değişmeler ve gelişmeler incelenmiştir. Çalışmaya temel oluşturan en önemli özellik, verilerin bizzat yerinde işletme sorumluları
    [Show full text]