DOCSLIB.ORG

(Simav-Kütahya) Cu-Pb-Zn-(Ag) Mineralization, NW TURKEY

Total Page：16

File Type：pdf, Size：1020Kb

Download full-text PDF Read full-text
(Simav-Kütahya) Cu-Pb-Zn-(Ag) Mineralization, NW TURKEY Cent. Eur. J. Geosci. • 5(3) • 2013 • 435-449 DOI: 10.2478/s13533-012-0139-2 Central European Journal of Geosciences Fluid Inclusion and Sulfur Isotope Thermometry of the Inkaya (Simav-Kütahya) Cu-Pb-Zn-(Ag) Mineralization, NW TURKEY Research Article Yeșim Özen∗ and Fetullah Arik† Geological Engineering Department, Selçuk University, Konya, Turkey Received 14 May 2013; accepted 18 August 2013 Abstract: The Inkaya Cu-Pb-Zn-(Ag) mineralization, located about 20 km west of the Simav (Kütahya-Turkey), is situated in the northern part of the Menderes Massif Metamorphics. The mineralization is located along an E-W trending fault in the Cambrian Simav metamorphics consisting of quartz-muscovite schist, quartz-biotite schist, muscovite schist, biotite schist and the Arıkayası formation composed of marbles. Mineralized veins are 30-35 cm in width. The primary mineralization is represented by abundant galena, sphalerite, chalcopyrite, pyrite, fahlore and minor amounts of cerussite, anglesite, digenite, enargite, chalcocite, covellite, bornite, limonite, hematite and goethite with gangue quartz. Fluid inclusion studies on the quartz samples collected from the mineralized veins indicate that the temperature range of the fluids is 235°C to 340°C and the salinities are 0.7 to 4.49 wt. % NaCl equivalent. The wide range of homogenization temperatures indicates that two different fluid generations were trapped in quartz. Sulfur isotope studies of the sulfide minerals showed that all of the δ S values are between − : and 2.6 per mil. These values are a typical range for hydrothermal sulfide minerals that have sulfur derived from a magmatic 34 source. 2 1 Pyrite-galena and pyrite-chalcopyrite sulfur isotope fractionation is consistent with an approach to isotopic equi- librium, and calculated temperatures are 254.6 and 277.4°C for pyrite-galena and 274.7°C for pyrite-chalcopyrite. The microthermometric data and sulfur isotope thermometry indicate the existence of a hydrothermal fluid that circulated along the fault crossing the Simav metamorphics and Arıkayası formation. Fluid inclusion and sulfur isotope thermometry can be used in combination with ore petrographical and geological information to provide site-specific targets for meso-hypothermal metal concentrations. Keywords: Fluid inclusion • sulfur isotope thermometry • Inkaya Cu-Pb-Zn-(Ag) mineralization • Simav • meso-hypothermal © Versita sp. z o.o. 1. Introduction ∗ † E-mail: [email protected] E-mail: [email protected] The study area is located in Ahmetli (Simav-Kütahya) in the Western Anatolia Region which is one of Turkey’s most important metallic provinces. The area is located in the western part of the Anatolian tectonic belt, in the south- ern part of the İzmir-Ankara zone, and in the northern 435 Fluid Inclusion and Sulfur Isotope Thermometry of the Inkaya (Simav-Kütahya) Cu-Pb-Zn-(Ag) Mineralization, NW TURKEY part of the Menderes Massif and it is part of the Inner volcano-sedimentary sequence affected by HP/LT meta- West Anatolian of the Aegean Region. The Inkaya Cu- morphism, and this blueschist belt rests with a tectonic Pb-Zn-(Ag) mineralization is located about 20 km west of contact on the Afyon Zone at the south [12]. The Afyon the Simav (Kütahya-Turkey) (Fig. 1). The İnkaya Cu-Pb- zone was overthrusted by the Tavşanlı Zone and con- Zn-(Ag) mineralization is located along the E-W trending sists of shelf-type metasediments of Paleozoic-Mesozoic fault in the Simav metamorphics and the Arıkayası forma- age affected by low grade, regional, greenschist metamor- tion belonging to Menderes Massif Metamorfics, is vein phism [2, 4, 12, 13]. The Afyon Zone rests directly on the type mineralization (Fig. 2, Fig. 3). gneisses of the Menderes Massif [8]. [14] suggested that The WNW-ESE trending Simav Graben is located in the the Afyon zone of the Anatolides uncomformably overlies study area (Fig. 2). The Simav Graben was formed due to the Menderes Massif mentioned as a “core complex”. [15] the activation of the lateral component of the Simav Fault suggested that the north-south shortening of NW Turkey by N-S extension [1]. Several mineralizations (Arpaçukuru ceased at the end of the Oligocene and is replaced by N- Fe-Cu, Değirmenciler Sb, Gürkuyu Sb, Pınarbaşı Fe- S extension in the Lower Miocene. Thus, the extensional Cu-Pb-Zn mineralizations etc.), occur along the Simav regime formed the E-W extending graben systems in the Graben, and were formed in association with a tectono- region [16, 17] (Fig. 1 and Fig. 2). The Menderes Massif magmatic period. is interpreted as a “metamorphic core complex” formed on Geological studies on the metamorphic rocks of the region account of the listric faults, e.g. [14], [18–23] which consti- were carried out by [2–4]. [5, 6] studied the granitoids from tute the boundary of the graben. The development of the the petrogenetic point of view. [7] investigated the chem- magmatic activity in the western Anatolia is closely asso- ical composition and origin of volcanic rocks of Cenozoic ciated with the tectonic evolution of the region [12, 17, 24– age in the Simav region. [8] determined that mineraliza- 33]. As a result of the N-S compressional tectonic regime, tion is related to the faults of the Simav Graben. [9] stud- calc-alkaline volcanism closely associated with the gran- ied five mineralizations in the region that are products of itoids was developed in the region. syn-extensional magmatism related to the Menderes core The Simav Graben trending WNW-ESE is located in the complex. study area (Fig. 2). The alluvium is commonly shown in The present study was carried out in order to investigate the north part of the Simav Graben, whereas metamorphic the chemical-physical conditions and formation tempera- and plutonic rocks commonly crop out in the south part tures of the hydrothermal fluids and the mechanism of the (Fig. 2). The region is crossed by E-W trending faults İnkaya Cu-Pb-Zn-(Ag) mineralization using isotopic and which are nearly parallel to the Simav graben fault. The fluid inclusion data. In this study, fluid inclusion and sul- other fault system is a N-S trending set which cut the fur isotope thermometry data along with field observations former set of faults. and ore petrographical data were interpreted to constrain chemical and temperature conditions of the mineralizing Pre-Cambrian Menderes Massif Metamorphics (Kalkan fluids in the İnkaya Cu-Pb-Zn-(Ag) mineralization. The formation, Simav metamorphics, Sarıcasu formation, study of the İnkaya Cu-Pb-Zn-(Ag) mineralization and Arıkayası formation) form the basement in the region similar mineralizations along Simav Graben will poten- (Fig. 2). The massive is composed of a Precambrian tially be used to resolve problems regarding other similar “Gneiss core” and Paleozoic and Mesozoic “schist cover” mineralizations in the world. series [34–36]. According to [14] the “Gneiss core” con- 2. Geological settings stitutes the base of the lithological units within the stud- ied area. It consists of the Kalkan formation represented 2.1. Regional geological setting by migmatite and biotite-bearing gneiss. The “schist cover” includes the Simav metamorphics, the Sarıcasu for- mation and the Arıkayası formation from bottom to top. Simav metamorphics which constitute the basal unit of The study area is located at the Menderes Massif (meta- the schist cover begin with muscovite schist, and con- morphic core complex) in the Western Turkey. In Western tinue with muscovite-biotite schist comprising metamafic- Turkey, the Pontides and the Anatolide-Tauride Block are metaultramafic levels in the middle part of the unit [8]. separated by an ophiolitic belt, known as the Izmir-Ankara The Sarıcasu Formation consists of quartz, albite, chlorite, suture zone, thrust southwards onto the Anatolides and muscovite bearing schists representing lower grade meta- Taurides [10] (Fig. 1). The region is within the Anatolides morphic facies than the Simav Metamorphics [8]. Arıkayası tectonic unit [11]. The Anatolides consist of the Tavşanlı formation has both lateral and vertical gradation to the zone, the Afyon zone and the Menderes Massif from north Sarıcasu Formation, the unit is composed of marble [8]. to south, respectively. The Tavşanlı zone consists of a The Budağan limestone unconformably overlies the meta- 436 Y. Özen, F. Arik Figure 1. Geological and geotectonical maps of the Western Anatolia (after [45]). morphics, starting with a conglomerate level including replacement-type kaolinite and alunite deposits related abundant and quartz pebbles. Granitoids crop out in the to the Simav Graben [8, 9, 37–44]. The İnkaya Cu-Pb-Zn- northern part of the studied area to the north of the Simav (Ag) mineralization, the Arpaçukuru Fe-Cu mineralization Graben. According to modal compositions of the Eğrigöz and the Değirmenciler Sb mineralization are shown along Granitoid, the pluton comprises granite, monzogranite and 2.2.the Simav Local Graben geological in Figure setting2. - ˙Inkaya deposit granodiorite, and is calc-alkaline in compositon [8,9]. The Kızılbük formation, uncomformably overlying the grani- toids, is composed of the alternation of sandstone, clay- stone, marl and clayey limestone, all of dirty yellow to Mesothermal base-metal (Cu-Pb-Zn) veins are located in beige colours [8]. The Kızılbük formation grades to the the northern block of the Simav Graben [46–49]. These Civanadağ tuffs and is related to the Akdağ volcanites. mineralizations occur in the Eğrigöz granitoids and in the The Civanadağ tuffs consist of white and gray coloured gneisses of the Menderes Massif. The İnkaya Cu-Pb- tuffs with agglomerates in the upper levels. The tuffs are Zn-(Ag) mineralization is a similar Cu-Pb-Zn vein in the rhyolitic, andesitic and dasitic in composition. The Ak- southern block of the Simav Graben. The mineralization dağ volcanites consist of andesite, rhyolite, rhyodacite and occurs in the “schist cover” of the Menderes Massif as a dacite [8,9] (Fig.2).
Load more

Recommended publications
  • Article Some Cryptognathid Mites (Acari: Cryptognathidae)
    Persian Journal of Acarology, Vol. 2, No. 3, pp. 487–502. Article Some cryptognathid mites (Acari: Cryptognathidae) from Kütahya Province (Turkey) İsmail Uluçay1* & Kamil Koç2 1 Hakkari University, Yüksekova Vocational School, Hakkari, Turkey; E-mail: iulucay @gmail.com 2 Celal Bayar University, Faculty of Sciences and Arts, Department of Biology, Manisa, Turkey. E-mail: [email protected] * Corresponding Author Abstract Six cryptognathid mites were collected from Kütahya Province. Of these, three species belong to the genus Cryptognathus Kramer, 1879 and three species to the genus Favognathus Luxton, 1973. A new species Cryptoganathus kutahyaensis sp. nov., and the male of Favognathus cucurbita Berlese, 1917, from Turkey, are described and illustrated. Keys to all the species of the genus Cryptognathus and the Favognathus species of the Kütahya Province are provided. Key words: Acari, Cryptognathidae, Cryptognathus kutahyaensis sp. nov., new species, Turkey. Introduction Cryptognathids are small, scarlet-red or orange mites, their measurments are from 300 to 400 µm in length. The body is oval and lacks a suture between the propodosoma and the hysterosoma. The dorsal shield is reticulate or punctate (Baker & Wharton 1952; Krisper & Schneider 1998; Luxton 1993). Their mouth parts are often highly protruding (Luxton 1973). Members of the family are generally collected from soil, grass-covered soil, litter, mosses and lichens and they feed on algae, mosses and fungi (Koç & Ayyıldız 1998; Doğan & Ayyıldız 2004; Doğan 2008; Doğan & Dönel 2010; Dönel & Doğan 2011; Luxton 1993; Swift 1996; Swift & Goff 2001). Cryptognathidae contains three genera: Cryptognathus Kramer, 1879, Favognathus Luxton, 1973 and Cryptofavognathus Doğan & Dönel, 2010. Nineteen species of genus Cryptognathus Kramer, 1879 have been so far recorded in the world and four of them are known from Turkey, namely, C.
    [Show full text]
  • Dumlupinar University International Relations Office Welcome Guide
    DUMLUPINAR UNIVERSITY INTERNATIONAL RELATIONS OFFICE WELCOME GUIDE CONTENTS Welcome to the Dumlupınar University………………………………………………………3 Turkey in Brief…………………………………………………………………………………4 Kütahya………………………………………………..……………………………………….5 Dumlupınar University………………………………………………………………………..7 Vision and Mission of Dumlupınar University………………………………………….……9 Faculties, Schools and Graduate Schools at Dumlupınar University………………………..10 Grading System at Dumlupınar University……………………………………………..…..13 International Relations Office………………………………………………………………..14 Useful Information……………………………………………………………………………15 Visa………………………...………………………………………………………....15 Residence Permit……………………………………………………………………...15 Health Insurance……………………………………………………………………...16 Cost of Living in Kütahya, Turkey…………………………………………………...17 Emergency Numbers………………………………………………………………….18 Phone Calls…………………………………………………………………………...18 Transportation………………………………………………………………………..19 Shops………………………………………………………………………………….19 Eating Out……………………………………………………………………………20 Leisure Time Activities & Entertainment……………………………………………20 Major Holidays in Turkey……………………………………………………………21 You should Know Before Coming to Kütahya, Turkey………………………………22 Survival Turkish……………………………………………………………………………...23 Notes………………………………………………………………………………………….26 2 DUMLUPINAR UNIVERSITY Welcome to the Dumlupınar University Dear incoming staff and students, First of all, we would like to thank you for your interest in performing an exchange study period at Dumlupınar University (DPU). This guide has been designed for foreign students
    [Show full text]
  • Hydrogeological, Hydrogeochemical and Isotope Geochemical Features of Thermal Waters in Simav and Environs
    PROCEEDINGS, Thirty-Ninth Workshop on Geothermal Reservoir Engineering Stanford University, Stanford, California, February 24-26, 2014 SGP-TR-202 Hydrogeological, Hydrogeochemical and Isotope Geochemical Features of Thermal Waters in Simav and Environs Olayinka A. BELLO1, Nevzat OZGUR2 and Tugba A CALISKAN3 1. Lagos, Nigeria. 2. Suleyman Demirel University, Department of Geological Engineering, Isparta, 32260, Turkey 3. Marmara Arastirma Merkezi, Center for Clean Production, Gebze-Kocaeli, Turkey. 1 [email protected], 2 [email protected], 3 [email protected] Keywords: Simav, Geothermal, Geothermometers, Hydrogeology, Hydrogeochemistry. ABSTRACT Simav geothermal field, one of Turkey’s most important fields, is located in Kütahya’s Simav graben system of western Anatolia. This is on the eastern part of the graben and approximately 4 km north of Simav town and on the NE edge of the Simav plain, which is separated from the mountain by a high and steep escarpment. The plain covers an area of about 70 km2 and is at an altitude of about 780 m asl and lies on latitude 390 5’ 23” N and longitude 280 58’ 46” E. The thermal waters of Simav can be classified as Na-HCO3-SO4 type water with the dominant cations in increasing order of Na+K>Ca>Mg while the anions are HCO3>SO4>Cl. The Cl-SO4-HCO3 ternary diagram shows that the waters are peripheral/immature and more likely related to groundwater heated by steam from deeper reservoirs. Quartz, aragonite, calcite and chalcedony are oversaturated at discharge temperatures while at a recomputed temperature according to the reservoir composition, only quartz, dolomite and chalcedony are oversaturated.
    [Show full text]
  • Simav Earthquake and Evaluation of Existing Sample RC Buildings According to the TEC-2007 Criteria
    EGU Journal Logos (RGB) Open Access Open Access Open Access Advances in Annales Nonlinear Processes Geosciences Geophysicae in Geophysics Open Access Open Access Nat. Hazards Earth Syst. Sci., 13, 505–522, 2013 Natural Hazards Natural Hazards www.nat-hazards-earth-syst-sci.net/13/505/2013/ doi:10.5194/nhess-13-505-2013 and Earth System and Earth System © Author(s) 2013. CC Attribution 3.0 License. Sciences Sciences Discussions Open Access Open Access Atmospheric Atmospheric Chemistry Chemistry and Physics and Physics 19 May 2011 Kutahya¨ – Simav earthquake and evaluation of Discussions Open Access Open Access existing sample RC buildings according to the TEC-2007Atmospheric criteria Atmospheric Measurement Measurement M. H. Arslan1, M. Olgun1, M. A. Koro¨ gluˇ 2, I. H. Erkan1, A. Koken¨ 1, and O. Tan1 Techniques Techniques 1 Department of Civil Engineering, Selcuk University, 42075 Konya, Turkey Discussions 2 Open Access Department of Civil Engineering, Necmettin Erbakan University, 42060 Konya, Turkey Open Access Correspondence to: M. H. Arslan ([email protected]) Biogeosciences Biogeosciences Discussions Received: 19 October 2012 – Published in Nat. Hazards Earth Syst. Sci. Discuss.: – Revised: 25 December 2012 – Accepted: 3 January 2013 – Published: 25 February 2013 Open Access Open Access Climate Abstract. This study examines the damage caused to rein- 7.2)) (Arslan and Korkmaz, 2007;Climate C¸agatay,˘ 2005; Inel et al., forced concrete structures by the 2011 earthquake that oc- 2008; Tan et al., 2008; Adalierof andthe Aydıng Pastun,¨ 2001; Sezen of the Past curred in Simav, Turkey. The study briefly reports on post- et al., 2003; Dogang˘ un,¨ 2004; Celep et al., 2011; Kaplan et Discussions earthquake field observations, tectonic characteristics of the al., 2004).
    [Show full text]
  • Employing Cantor Sets for Earthquake Time Series Analysis in Two Zones of Western Turkey
    View metadata, citation and similar papers at core.ac.uk brought to you by CORE provided by Elsevier - Publisher Connector Scientia Iranica A (2012) 19 (6), 1456–1462 Sharif University of Technology Scientia Iranica Transactions A: Civil Engineering www.sciencedirect.com Employing Cantor sets for earthquake time series analysis in two zones of western Turkey A. Sezer ∗ Department of Civil Engineering, Ege University, Insaat Muhendisligi Bolumu, 35100, Bornova Izmir, Turkey Received 24 April 2012; revised 30 August 2012; accepted 6 October 2012 KEYWORDS Abstract In this study, a fractal approach is employed to analyze the seismic history of Fethiye and Fractal approach; Simav zones in the West of Turkey. In this scope, a database, including the set of earthquakes in two Aegean region; seismogenic zones, is compiled. Applying fractal dimension and probability concepts, it is aimed to find out Earthquakes; the occurrence probability of earthquakes having magnitudes equal to or greater than a threshold level. Cantor sets. The results are analyzed in detail and relationships among the fractal dimension, threshold magnitude, probability intercept, and critical time scale are presented. The analyses revealed that activities in the Fethiye Zone are more frequent and continuous than those in the Simav Zone. As mentioned in previous studies, the critical time scales at certain magnitude thresholds can be referred to as the lower limit of the recurrence period of earthquakes in these zones. ' 2012 Sharif University of Technology. Production and hosting by Elsevier B.V. Open access under CC BY-NC-ND license. 1. Introduction clustering occurs with fractal dimension D, when fraction x of the intervals of length τ containing earthquakes is directly Engineering knowledge in the 21st century is able to analyze proportional to τ 1−D .0 < D < 1/.
    [Show full text]
  • Cancer and Death Ratio Maps Case Study of Kutahya Province in Turkey
    The International Journal of Engineering and Science (IJES) || Volume || 6 || Issue || 12 || Pages || PP 15-20 || 2017 || ISSN (e): 2319 – 1813 ISSN (p): 2319 – 1805 Cancer And Death Ratio Maps Case Study of Kutahya Province in Turkey Hatice Canan Gungor Necmettin Erbakan University, Faculty of Aeronautics and Astronautics, Department of Space and Satellite Sciences, Konya Corresponding email: [email protected] --------------------------------------------------------ABSTRACT----------------------------------------------------------- Nowadays, the boundaries of science disciplines all over the world are constantly evolving. Therefore, common issues arise between disciplines, which can solve them together more healthily. In this framework, Geographical Information Systems (GIS), keeping the developing technologies within the scope, is serving to a wide spectrum by constantly renewing and developing itself. GIS is a technological system consisting of computer software and hardware that visualize and analyze the wide range of information in the geographical context. This system has almost all the features of a database management system. The core data in the Geographical Information System is necessarily related to the geographical location. Especially in recent years, there has been a significant increase in GIS applications in medical matters. GIS supports the day-to-day operations of large-scale to small-scale public health programs, and their managerial work with the holistic perception ability that they provide through planning contributions and epidemiological maps. The relationship between medical science and GIS technology has begun with approaches that have been put forward in order to carry out the studies on medical geography more effectively. There have been many international studies on the use of GIS in medical geography. To benefit from this technology in the field of health care, two spatial analysis approaches have been used.
    [Show full text]
  • 19 Mayıs 2011 KÜTAHYA-SİMAV DEPREMİ
    KANDİLLİ RASATHANESİ VE DEPREM ARAŞTIRMA ENSTİTÜSÜ 19 Mayıs 2011 KÜTAHYA-SİMAV DEPREMİ Hazırlayanlar; Dr. Can Zülfikar Araş. Gör. Yaver Kamer Araş. Gör. Eren Vuran Haziran, 2011 İSTANBUL 1 İçindekiler İçindekiler ............................................................................................................................................... 2 Şekillerin Listesi ..................................................................................................................................... 3 Tabloların Listesi .................................................................................................................................... 7 1 Giriş .. 8 2 Bölgenin Genel Jeolojisi .................................................................................................................. 12 3 Bölgenin Sismotektonik Özellikleri ................................................................................................ 14 4 Depremin Kaynak Parametreleri ..................................................................................................... 17 5 Depremin İstatistik Yönden Özellikleri ........................................................................................... 18 6 Deprem Sarsıntı ve Hasar Tahminleri ............................................................................................. 20 7 Kuvvetli Yer Hareketi Kayıtları ...................................................................................................... 22 8 Bina Tipleri .....................................................................................................................................
    [Show full text]
  • Il Içi Atama 30072020.Xls
    KÜTAHYA İL MİLLÎ EĞİTİM MÜDÜRLÜĞÜ 2020 YILI ÖĞRETMENLERİN İL İÇİ İSTEĞE BAĞLI YER DEĞİŞTİRME SONUÇLARI Sıra Adı Soyadı Alanı Hizmet Puanı Eski Görev Yeri Atandığı Okul-Kurum Adı Domaniç / Domaniç Şehit Ömer Halisdemir 1 FAZLI KARABULUT Almanca 142 Merkez - Kılıçarslan Anadolu Lisesi Anadolu Lisesi 2 NİMET GENCER Almanca 73 Merkez / Kütahya Lisesi Merkez - Kılıçarslan Anadolu Lisesi Domaniç / Domaniç Şehit Ömer Halisdemir 3 ÜLKÜ YAVUZ Almanca 64 Aslanapa - Aslanapa Anadolu Lisesi Anadolu Lisesi Merkez - Kütahya Kız Anadolu İmam Hatip 4 MUSTAFA GENÇ Arapça 291 Merkez / Ertuğrul Gazi İmam Hatip Ortaokulu Lisesi Merkez - Yavuz Sultan Selim Özel Eğitim 5 ALİ EFE Beden Eğitimi 137 Merkez / Seyitömer Ortaokulu Uygulama Okulu III. Kademe 6 ALİ ZENGİN Beden Eğitimi 263 Merkez / 30 Ağustos Ortaokulu Merkez - Dumlupınar Ortaokulu 7 MURAT KOÇAK Beden Eğitimi 322 Simav / Nurullah Koyuncuoğlu Anadolu Lisesi Simav - Simav Anadolu Lisesi Merkez - Fethi Güzen İşitme Engelliler 8 MUSA MERCAN Beden Eğitimi 138 Aslanapa / Ortaca Ortaokulu Ortaokulu 9 YILMAZ SATILMIŞ Beden Eğitimi 82 Merkez / Kızılcaören Ortaokulu Aslanapa - Ortaca - Ortaca Ortaokulu Tavşanlı - Tavşanlı Şeyh Edebali İmam-Hatip 10 YUNUS EROĞLU Beden Eğitimi 150 Tavşanlı / Tunçbilek Atatürk Ortaokulu Ortaokulu Merkez - Kütahya Kız Anadolu İmam Hatip 11 NURSEL DURMAZ Bilişim Teknolojileri 221 Merkez / İsmet İnönü Ortaokulu Lisesi Gediz - Gediz Selçuklu Mesleki ve Teknik 12 AYÇA TÜLÜOĞLU Biyoloji 278 Pazarlar / Pazarlar Anadolu Lisesi Anadolu Lisesi 13 NACİYE YAZICI Biyoloji 295 Merkez / Fatih
    [Show full text]
  • Gediz-Kütahya-NW Turkey)
    Cumhuriyet Üniversitesi Fen Fakültesi Cumhuriyet University Faculty of Science Fen Bilimleri Dergisi (CFD), Cilt 37 (2016) Science Journal (CSJ), Vol. 37 (2016) ISSN: 1300-1949 ISSN: 1300-1949 http://dx.doi.org/10.17776/csj.17489 Mineralogy, Geochemistry and Stable Isotope Investigation of Gürkuyu Sb Mineralization (Gediz-Kütahya-NW Turkey) Yeşim ÖZEN, Fetullah ARIK Department of Geological Engineering, Selçuk University, 42079 Konya, Turkey Received: 16.09.2016; Accepted: 18.11.2016 Abstract. The Gürkuyu Sb mineralization is located in the western part of Anatolian tectonic belt, in southern part of İzmir- Ankara zone and in northern part of Menderes Massif. The mineralization located at west of the Koca hill in east of Gürkuyu village of Gediz (Kütahya-Turkey) has been characterized through the detailed examinations involving sulfur and oxygen isotope. Serpentinites of Dağardı melange and crystallized limestones of Budağan limestone were hydrothermally altered by hydrothermal solutions, come from fissures and fractures due to tectonic movement during the thrust of melange and occurred silicified zone. Gürkuyu Sb mineralization suggest that occurred in this silicified zone. In Gürkuyu mineralization, primary ore minerals are antimonite and pyrite, secondary ore minerals are senarmontite, valentinite, orpiment and realgar. Quartz and calcite are the most common gangue minerals. In mineralization, average contents of Fe2O3, Sb, Hg, As and Au are 2.15 wt.%, 13359 pm, 1.12 ppm, 1367 ppm and 163.82 ppb, respectively. In Gürkuyu Sb mineralization, δ34S values of stibnite are ranged from 1.0 ‰ to 1.3 ‰. δ18O values of quartz are ranged is 15.8 ‰ in Gürkuyu mineralization. Sulfur and oxygen isotope values are similar to the values for magmatic rocks and to the values for fluids of magmatic origin.
    [Show full text]
  • T.C. Kütahya Il Özel Idaresi
    T.C. KÜTAHYA İL ÖZEL İDARESİ BRİFİNG DOSYASI - 2009 - İÇİNDEKİLER SAYFA 01. - İnsan Kaynakları ve Eğitim Müdürlüğü..………………………………....................4 02. – Destek Hizmetleri Müdürlüğü…………….……………............................................7 03. – Yazı İşleri Müdürlüğü ……………….………….…...................................................9 04. – Mali Hizmetler Müdürlüğü………………………………………………………….10 05. – Bilgi İşlem Müdürlüğü…………………………………………………………….. 17 06. – Yol ve Ulaşım Hizmetleri Müdürlüğü……….…………………………..……….... 18 07. – Su ve Kanal Hizmetleri Müdürlüğü……................................................................... 25 08. – İmar ve Kentsel İyileştirme Müdürlüğü..................................................................... 32 09. – Ruhsat ve Denetim Müdürlüğü…………………………………………….………. 33 10. – Kültür ve Sosyal İşler Müdürlüğü………………………………………………….. 35 11 – KÖYDES 2009 Yılı Programı………………………………………………............ 38 12 – KÖYDES 2005-2006-2007-2008 Yılları Uygulamaları…….……………………….42 13 – Gayrimenkul İcmal Tablosu……………………….………………………………. 50 1 Kütahya ve İlçeleri arasındaki uzaklıklar ( Km) İlçe Bazında Köy Nüfusu, Köy Sayısı, Yüzölçümü ve Yükseklik İl Köy Köy Köy Sayısı YüzölçümüYüzölçümüne Yükseklik Nüfusu Sayısı Oranı % (km²) Oranı (%) (m) MERKEZ 21.614 114 22,2 2.572 22 969 ALTINTAŞ 11.000 33 6,4 905 8 1020 ASLANAPA 9.894 33 6,4 659 6 950 ÇAVDARHİSAR 5.239 22 4,2 591 5 945 DOMANİÇ 10.043 31 6 619 5 900 DUMLUPINAR 1.844 10 1,9 305 3 1222 İLÇE EMET 7.594 29 5,6 684 6 750 GEDİZ 12.995 47 9,1 1468 12 736 HİSARCIK 5.873 21 4 330 3 785 PAZARLAR 1.535 6 0,1 144 1 810 SİMAV 17.738 69 13,4 1557 13 820 ŞAPHANE 2.545 10 1,9 251 2 950 TAVŞANLI 22.520 88 17,1 1804 15 860 Toplam 130.434 513 100 11,889 100 2 Misyonumuz Sahip olduğu kaynakları etkin bir biçimde kullanıp, yöre halkının beklentilerine uygun kaliteli hizmetler sunarak kırsal ve kentsel kalkınmayı sağlamaktır.
    [Show full text]
  • Neotectonics and Seismicity of Eastern Simav Graben, Kütahya – Turkey a Thesis Submitted to the Graduate School of Natural A
    NEOTECTONICS AND SEISMICITY OF EASTERN SİMAV GRABEN, KÜTAHYA – TURKEY A THESIS SUBMITTED TO THE GRADUATE SCHOOL OF NATURAL AND APPLIED SCIENCES OF MIDDLE EAST TECHNICAL UNIVERSITY BY MUSTAFA KAPLAN IN PARTIAL FULFILLMENT OF THE REQUIREMENTS FOR THE DEGREE OF MASTER OF SCIENCE IN GEOLOGICAL ENGINEERING SEPTEMBER 2014 Approval of the thesis: NEOTECTONICS AND SEISMICITY OF EASTERN SİMAV GRABEN, KÜTAHYA – TURKEY submitted by MUSTAFA KAPLAN in partial fulfillment of the requirements for the degree of Master of Science in Geological Engineering Department, Middle East Technical University by, Prof. Dr. Canan Özgen _____________________ Dean, Graduate School of Natural and Applied Sciences Prof. Dr. Erdin Bozkurt _____________________ Head of Department, Geological Engineering Prof. Dr. Ali Koçyiğit _____________________ Supervisor, Geological Engineering Dept., METU Examining Committee Members: Prof. Dr. Erdin Bozkurt _____________________ Geological Engineering Dept., METU Prof. Dr. Ali Koçyiğit _____________________ Geological Engineering Dept., METU Prof. Dr. F. Bora Rojay _____________________ Geological Engineering Dept., METU Prof. Dr. Reşat Ulusay _____________________ Geological Engineering Dept., HÜ Assist. Prof. Dr. A. Arda Özacar _____________________ Geological Engineering Dept., METU Date: 03.09.2014 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. Name, Last Name: Mustafa Kaplan Signature: iv ABSTRACT NEOTECTONICS AND SEISMICITY OF EASTERN SİMAV GRABEN, KÜTAHYA – TURKEY Kaplan, Mustafa M.S., Department of Geological Engineering Supervisor: Prof. Dr. Ali Koçyiğit September 2014, 121 pages The Simav graben is an about 1-9 km wide, 50 km long and approximately WNW- trending active depression.
    [Show full text]
  • Flooding and Earthquake Risk Interpretation for Kutahya Province, Turkey, Using ASTER DEM
    Journal of Geography and Geology; Vol. 6, No. 3; 2014 ISSN 1916-9779 E-ISSN 1916-9787 Published by Canadian Center of Science and Education Flooding and Earthquake Risk Interpretation for Kutahya Province, Turkey, Using ASTER DEM Umut Erdem1 & Ali Can Demirkesen1 1 Department of City & Regional Planning, Izmir Institute of Technology, Izmir, Turkey Correspondence: Umut Erdem, Department of City & Regional Planning, Izmir Institute of Technology, Izmir, Turkey. Tel: 90-232-750-7092. E-mail: [email protected] Received: May 29, 2014 Accepted: June 30, 2014 Online Published: July 23, 2014 doi:10.5539/jgg.v6n3p133 URL: http://dx.doi.org/10.5539/jgg.v6n3p133 Abstract Kutahya Province is a significant cultural heritage area of Turkey; it is susceptible to flooding when sudden heavy rain falls and is located in a high-risk earthquake region. The objective of this study was to acquire geo-information from Kutahya Province and interpret the risk levels to the population from floods and earthquakes. In this study, the Advanced Space-borne Thermal Emission Reflection Digital Elevation Model of Kutahya Province was used to create maps that illustrate the digital terrain model and the 3D fly-through dynamic model of the study region. The maps exhibit landform characteristics, fault zones, earthquake locations, thermal locations, stream drainages and water-flow accumulation areas. From the interpretation of the maps, the results revealed that the most susceptible areas to flooding are the settlements and agricultural plains of Kutahya, Altintas, and Simav, in decreasing order. Gediz, Simav, Kutahya, Emet, Tavsanli, Dumlupinar, Domanic, Hisarcik, Pazarlar and Saphane are at high risk of earthquake damage, in decreasing order.
    [Show full text]