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Türkiye Jeoloji Bülteni

Türkiye Jeoloji Bülteni

2012 NİSAN Cilt 55 Sayı 2
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(Paleogene Molluscan Fauna and Biostratigraphy Between Kuscu and Macun village, Temelli (SW Ankara)
Müjde Gürsoy Güler Taner
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Abstract: In this study, paleontological and biostratigraphic characteristics of the Paleogene geologic unitsoutcropping between Kuscu and Macun villages located around Temelli district, Polatli, Ankara. We haveexamined the patterns of Pelecypoda and Gastropoda samples. Seven measured stratigraphic sectionfrom the west of Macun village to east of Kuscu village, which contains the Pelecypoda and Gastropodapatterns, reach total thickness of 52 metres. As a result of field studies, seven species belongs to class ofPelecypoda and one of the new sixteen species belongs to class of Gastropoda have been described. Considering paleogeographic distribution and biostratigraphy of described fauna, it is quite proper topropose that they represent Thanetian age and can be interpreted as belonging to Kırkkavak Formation.Furthermore, the paleoecologic characteristics of the fauna strongly suggests that the shallow andtemperate coastal marine facial conditions were prevalent at the region during that time span.

  • Biostratigraphy

  • Gastropoda

  • Pelecypoda

  • Paleogene

  • Paleontology


  • Akarsu, İ.,1959. Ankara Bölgesi, Polatlı ve civarının Petrol Jeolojisi, MTA Dergisi, Sayı: 52, s. 99-106, Ankara.

  • Akarsu, İ., 1971. Polatlı – Haymana civarının detay petrol jeolojisi: T.P.A.O. raporu 2502 (yayımlanmamış), Ankara.

  • Bayan. J.F., 1873. Notes sur quelques fossiles tertiaires, p.91-136, pl.XIII-XV, Paris.

  • Baykal, F.,1948. Paleontoloji, Omurgasız Fosiller, İstanbul Üniversitesi Yay. Sayı:384, 328 s., İstanbul.

  • Bellardi, L., 1852. Catalogue raisonné des fossiles nummulitiques du comte de Nice. M.S.G.Fr., sér.Iı, vol. IV, p. 205-300, pl. XII-XXII, Paris.

  • Bontscheff, St., 1896. das Tertiärbecken von Haskovo (Bulgarien). Jahrd. d. k. k. Geol. Reichsanst, Bd.46, Heft 2, p.309-384, Taf. III-IV, Wien.

  • Boussac, J., 1911 a. Études Paléontologiques sur le Nummulitique Alpin, Texte, 438 p., Paris.

  • Boussac, J., 1911 b. Études Paléontologiques sur le Nummulitique Alpin, Atlas, 118 p., I-XXII pl., Paris.

  • Cossmann, M., 1889. Catalogue illustré des coquilles fossiles de l’éocéne des environs de Paris, fasc.4, Soc. Royale Malac. de Belgique, 385 p., 12 pl. Bruxelles.

  • Cossmann, M., 1899. Mollusques Éocéniques de la Loire-Inférieure, Bull. De la Soc. des Sc. Nat. de l’Ouest de la France, T.2, Nantes.

  • Cossmann ve Pissarro,1900. Fauna Éocénique du Cotentin (Mollusques), Bull. de la Soc. Geo. De Normandie, T. I, p.295, t.I-XXI, Le Havre.

  • Cossmann, M., 1901. Essais de Paléoconchologie Comparée, T.IV, 293 p., 10 pl, Paris.

  • Cossmann, M., 1903. Esseis de Paléoconchologie Comparée, T.V, 215 p., 9 pl., Paris.

  • Cossmann, M., 1904. Essais de Paléoconchologie Comparée, T.VI, 151 p., 9 pl, Paris.

  • Cossmann ve Pissarro, 1904-06. Iconographie compléte des coquelles fossiles de l’éocéne des environs de Paris, t.I, Pelecypodes, 45 pl., Paris.

  • Cossmann, M., 1906. Essais de Paléoconchologie Comparée, T.VII, 261 p., 14 pl., Paris.

  • Cossmann, M., 1908. Les Pelecypodes du Montien de Belgique. Mem. Mus. Royal d’Hist. Nat. De Belgique, T.V, 76 p., 8pl, Bruxelles.

  • Cossmann ve Pissarro, 1911. Inoconographie copléte des coquilles fossiles de l’éocéne des environs de Paris. T.II, 45 pl., Paris.

  • Deshayes, G.P., 1860. Descriptions des animaux sans vertebres decouverts dans le bassin de Paris, T.I, 912 p., 89 pl., Paris.

  • Deshayes, G.P., 1864. Descriptions des animaux sans vertebres decouverts dans le bassin de Paris, T.II, 968 p., pl.1-64, Paris.

  • Eames, F.E., 1952. A contribution to the study of the eocene in Western Pakistan and Western India. C. The discription of the Scaphopoda and gastropoda. Phyl. Trans. Of the Royal Soc. Of London, ser. B, vol.236, No:631, 168 p., 6 pl., London.

  • Fabiani, R., 1908. Paleontologia dei Colli Berici, p.45-247, pl.I-VI, İtalya.

  • Farchad, H., 1936. Etude du Thanetien (Landinien marin) du Bassin de Paris. M.S.G.Fr., Nouv.ser.13, Mem.30, p.5-101, pl.6, Paris.

  • Favre, J., 1914-18. Catalogue illustré de la collection Lamarck. Mus. d’Hist. Nat. de Genéve, 112 pl., Genéve.

  • Frauscher, K.F., 1886. Das unter-eocän Nordalpen und seine Fauna I.Theil, Lamellibranchiata. Denkschr. d. k. Ak. d. Wiss., math.-naturw., p.37-270, pl.I-XII, Wien.

  • Fuchs, Th., 1869. Die Conchylienfauna der Eocänbildungen von Kalinowka im gouvernement Chersan im Südlichen Russland. P. 1-24, pl. I-V, Petersburg

  • Furon ve Soyer, 1947.Catalogue des fossiles tertiaires du Bassin de Paris. Savoir en Hist. Natur., vol. XXII, 240 p., 32 pl., Paris.

  • Gmelin, J.F., 1791. Systema Naturae, Caroli a Linné, systema naturae. Tom. I. Pars VI. - pp. 3021-3910. Lipsiae.

  • Glibert, M., 1936. Fauna malacologique des sables de Wemmel I Pelecypodes. Mem.du Mus. Royal d’Hist. Nat. de Belgique No.78, 242 p., 75 textfigs, 7 pl., Bruxelles.

  • Hébert ve Renevier, 1854. Description des fossiles du terrain nummulitique suppérieur des environs de Gap, des Diablerets et de quelques localités de la Savoie. Bull. De la Soc. Statist. De l’Isére, 1854; (2), III, 88 p., 2 pl., Grenoble.

  • Karagiuleva, J.D., 1964.Les Fossiles de Bulgarie, Paléogéne Mollusca, 270 p., LVII Taf., Sofia.

  • Mayer-Eymar, C., 1895, Description de coquelles fossiles des terrains tertiaires inferieurs (suite). Journ. Conch. Sér.3e, vol. XLIII, p. 40-54, pl. II-III, Paris.

  • McKerrow, W.S., 1978. The Ecology of Fossils, 383 p.,Duckworth, London.

  • Mészăros, N.,1957. Biblioteca de Geologie şi Paleontologie - I, Fauna de Molluşte a Depozitelor Paleogene din NordVestul Transilveniei, 174 p., 33 pl., Bucureşti, Romine.

  • Moore, R.C., 1964-1969. Tretise on Invertebrate Paleontology, Mollusca 6 Bivalvia, 489p., The University of Kansas, USA.

  • Oppenheim, P., 1901. Über einige alttertiäreFaunen der österreiechisch – ungarischen Monarchie. Beitr. Z. Pal. Und geol. Österr. Ungarns und des Orients, Bd. XIII, p.145-227, t.XI-XIX, Wien-Leipzig.

  • Oppenheim, P., 1906. Neue Beiträge zur Geologie und Paleontologie der Balkanhalbinsel. Zeitschr. d. d. g. Ges., Bd.58, p.109- 180, textfigs.8, T.VIII, Berlin.

  • Orbigny, A., d’, 1850. Prodrome de Paléontologie stratigraphieque universelle des animaux Mollusques et Rayonnes. T.II, 427 p., Paris.

  • Reckamp, J.U. ve Özbey, S., 1960. Petroleum Geology of Temelli and Kuştepe strauctures, Polatli area: Petrol İşl. Gnl. Md., Ankara (yayımlanmamış).

  • Rigo de Righi, M ve Cortesini, A., 1960. Regional studies Anatolian basin, progress report 1, Turkish Gulf Oil Company: Petrol İşl. Gnl. Md., (Gulf-Mobil 1958-1961 yılları arasında yapılan çalışmalar) Ankara (yayımlanmamış).

  • Schlosser, M., 1925. Die Eocänfauna der bayerischen Alpen. I Teil. Die Fauna des Unter und Mitteleocän; II Teil: obereocänfauna, Abh. d. Bayer. AK. d. Wiss. Math. nat. Abt.30, Bd. 7, p. 1-207; p. 11-68, 8 taf, München.

  • Stchépinsky, V., 1946. Türkiye ‘nin Karakteristik Fosilleri, MTA Yayınları, No:1, 151 s., 37 lev., Ankara.

  • Sirel, E., 1975. Polatlı (GB Ankara) güneyinin stratigrafisi, Türkiye Jeoloji Kurumu Bülteni, c.18, 181-192, Ankara.

  • Sirel, E., ve Gündüz, H.,1976. Haymana (G Ankara) yöresindeki İlerdiyen, Küiziyen ve Lütesiyen› deki Nummulites, Assilina ve Alveolina cinslerinin bazı türlerinin tanımlamaları ve stratigrafik dağılımları, Türkiye Jeoloji Kurumu Bülteni, c.19,1, 31-44, Ankara.

  • Sirel, E., Dağer, Z., Sözeri, B., 1986. Some Biostratigraphic and Paleogeographic observations on the Cretaceous / Tertiary Boundary in the Haymana - Polatlı region in:walliser, Global Bio-Events, Lecture notes in Earth Sciences, V.8, 385-396, Berlin, Heidelberg.

  • Tchihatcheffi, P.de, 1866-69. Asie Mineure, Description Physique, Paleontologie, Text et Atlas, p.110-232, pl. I-XX, Paris.

  • Turkish Gulf Oil Company, 1961. Orta Anadolu’da Tuz Gölü baseninin bölgesel jeolojisi ve yapılan petrol aramaları. Petrol Faaliyeti, 31-33.

  • Toker, V., 1979. Haymana yöresi (GB Ankara) Üst Kretase Planktonik Foraminifera› ları ve biyostratigrafi incelemesi, Türkiye Jeoloji Kurumu Bülteni, c.22, 121-134, Ankara.

  • Taner, G., 1994. Paleoekoloji İlkeleri, TMMOB Yay. No:37, 337s., Ankara.

  • Ünalan, G., Yüksel, V., Tekeli, T., Gönenç, O., Seyirt, Z., Hüseyin, S., 1976. Haymana-Polatlı yöresinin (GB Ankara) Üst Kretase-Alt Tersiyer stratigrafisi ve paleocoğrafik evrimi, Türkiye Jeoloji Kurumu Bülteni, c.19,159-176, Ankara.

  • Vincent, E., 1930. Etudes sur les Mollusques Montiens du poudingue et du tufeau de Ciply. Mem. Du Mus. Royal l’Hist. Natur. de Belgique Mem. No:46, 115 p., 37 textfigs, 6 pl, Bruxelles.

  • Wenz, W., 1938-43. Gastropoda, Handbuch der Palaozoologie, 1-2 c., 1639 p.,Berlin.

  • Gürsoy, M , Taner, G . (2012). Kuşçu ve Macun Köyleri Arası Paleojen Mollusk Faunası ve Biyostratigrafisi, Temelli (GB Ankara) . Türkiye Jeoloji Bülteni , 55 (2) , 57-86 . Retrieved from https://dergipark.org.tr/tr/pub/tjb/issue/28143/299121

    • Digital geologic mapping and ASTER image analysis in the southern part of the Tecer Mountains on the Inner Tauride Suture
    Mustafa Yakan Kaan Şevki Kavak Haluk Temiz
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    Abstract: This study is aimed to perform digital geologic mapping and ASTER image analysis around southeasternpart of the Sivas Tertiary Basin. The interest area is located at the intersection of ENE-WSW orientedDeliler Thrust Belt and Tecer Fault Zone. Ophiolithic rocks which were belonging to Inner TaurideOcean Suture belt were outcropped in a vast region. This region also forms the northern boundary of theMenderes-Tauride platform. Tectonostratigraphy of the region is represented by two different sedimentarysequences separated by Deliler Fault Zone. While a thick cover of Oligocene-Miocene continental unit wasobserved on the southern section of Deliler Fault Zone, Lower-Middle Eocene marine, Oligocene gypsumand Lower Miocene marine sediments were outcropped on the northern part of this belt. Late Miocenecontinental deposits were folded while Plio-Quaternary fluvial sediments were observed horizontallyalong the Deliler Thrust Zone. Within the context of this study, interested region was mapped digitallyusing tablet pc and ArcPad software. Using this software, areas of outcropping units, linear geologic mapelements like faults and fold axes were recorded digitally during field studies and some database queriessuch as formation name, age, and lithologies were determined in terms of saving time and digitizationefforts. Additionally, a number of image processing efforts were applied to 14 channels ASTER image ofthe region to highlight geological features such as lithological boundaries and structural components.Thus, a detailed digital geologic map was formed at the end of this search. Furthermore, a number ofimage processing studies were acquired supporting geological mapping at field.  

  • ASTER

  • Deliler Thrust Zone

  • digital geologic map

  • digital image processing

  • remote sensing

  • Sivas Tertiary Basin

  • Tablet pc


  • Abera, G.B., (2005), “Application of Remote sensing and Spatial Data Integration Modeling to Predictive Mapping of Apatite-Mineralized zones in the Bikilal Layered Gabbro Complex, Western Ethiopia”, International Institute for Geo-Information Science and Earth Observation Enschede, The Netherlands.

  • ASTER Users Guide, Parth II, 2005, ver. 4.

  • Bierwirth, P.N., Blewett, R. S., and Huston, D. L., 2002, Hyperspectral mapping of mineral assemblages associated with gold mineralization in the West Pilbara, W.A. Economic Geology, 97: 4, 819-826.

  • Clegg, P., Bruciatelli, L., Domingos, F., Jones, R. R., De Donatis, M., Wilson, R. W., 2006. Digital geological mapping with tablet PC and PDA: A Comparison. Computers & Geosciences 32, 1682-1698.

  • De Donatis, M., Bruciatelli, L., 2006. MAP IT: The GIS software for field mapping with tablet pc. Computers & Geosciences 32, 673–680.

  • Edmondo G. P., 2003. Digital Geologic Field Mapping Using Arcpad, Digital Mapping Techniques ‘02 -- Workshop Proceedings U.S. Geological Survey Open-File Report 02-370.

  • Erdas Field Guide, (2003), Seventh Edition, Leica Geosystems GIS & Mapping, LLC, Atlanta, Georgia, USA.

  • Gad, S. ve Kusky, T., 2007. ASTER spectral ratioing for lithological mapping in the Arabian_Nubian shield, the Neoproterozoic Wadi Kid area, Sinai, Egypt, Gondwana Research, 11, 326-335.

  • Gomez C., Delacourt C., Allemand P., Ledru P., Wackerle R., 2005. Using ASTER remote sensing data set for geological mapping, in Namibia. Physics and Chemistry of the Earth 30 , 97–108.

  • Gökten, E., 1993. Ulaş (Sivas) doğusunda Sivas Havzası güney kenarının jeolojisi: İç Toros Okyanusu’nun kapanımıyla ilgili tektonik gelişim, TPJD Bülteni, V.5/1. 35-55.

  • Hewson., R.D., Cudahy, T.J., Huntington, J.F., 2001 Geologic and alteration mapping at Mt Fitton, South Australia, using ASTER satellite-borne data., IEEE 2001 International Geoscience and Remote Sensing Symposium, 9–13 July (2001).

  • Hewson, R.D., Cudahy, T.J., Brutt, A.C., Okada, K. and Mauger, A.J., 2004, Assessment of geological mapping potential using ASTER imagery within the Broken Hill and Olary domains. In:12th Australasian Remote Sensing and Photogrammetry Conference, Perth, 2004. Proceedings, p. 12.

  • Kalinowski A. ve Oliver S., 2004. ASTER Mineral Indekx Processing Manual, Remote Sensing Applications Geoscience Australia.

  • Mobile Mapper 6, MakroPad, MakroMap Kullanıcı Başvuru Rehberi, Geomatics Hrt. Müh ve Müş. Ltd. Şti.

  • Ninomiya, Y., 2002. Mapping quartz, carbonate minerals and maficultramafic rocks using remotely sensed multispectral thermal infrared ASTER data. P SPIE, 4710, pp. 191-202.

  • Okay, A.Ü. & Tüysüz, O. 1999. Tethyan sutures of northern Turkey. In: DURAND, B. JOLIVET, L. HORVTH, F. & S.RANNE, M. (eds), The Mediterranean Basins: Tertiary Extension Within the Alpine Orogen. Geological Society, London, Special Publications 156, 475-515.

  • Öztan, S. ve Süzen, L., 2011, Mapping evaporate minerals by ASTER, International Journal of Remote Sensing,, 32-6, 1651-1673.

  • Pena, S.A., and Abdelsalam, M.G. 2006. Orbital remote sensing for geological mapping in southern Tunisia: Implication for oil and gas exploration. Journal of African Earth Sciences – Remote Sensing for Africa. 44, 203-219.

  • Rowan, L. C., Mars, J. C., 2003. Lithologic mapping in the Mountain Pass, California area usingAdvanced Spaceborne Thermal Emission and Reflection Radiometer (ASTER) data, Remote Sensing of Environment 84, 350–366.

  • Sağıroğlu, A., 2004. Ulaş (Sivas) batısında Deliler fayının tavan bloğunun tektonik deformasyon biçimi ve kinematiği, Cumhuriyet Üniversitesi Fen Bilimleri Enstitüsü, Yüksek Lisans Tezi, 60.

  • Şengör, A.M.C. ve Yılmaz, Y., 1981. Tethyan evolution of Turkey: A plate tectonic approach. Tectonophysics, 75, 181-241.

  • Volesky, J.C., Stern., R.J. ve Johnson., P.R., 2003, Geological control of massive sulphide mineralization in the Neoproterozoic Wadi Bidah shear zone, southwestern Saudi Arabia, inferences from orbital remote sensing and field studies, Precambrian Research, 123, 235-247.

  • Yakan, M , Kavak, K , Temiz, H . (2012). İç Torid Kenedinin Tecer Dağları (Sivas) Güneyindeki Kesiminin Sayısal Jeolojik Haritalanması ve ASTER Görüntüleriyle Analizi . Türkiye Jeoloji Bülteni , 55 (2) , 87-110 . Retrieved from https://dergipark.org.tr/tr/pub/tjb/issue/28143/299131

    • Fluid Inclusion Data On Quartz and Calcite In Alteration Zones of Polymetallic Mineralizations at Mayıslar Area (Sarıcakaya-Eskişehir, Turkey)
    Banu Parlak İbrahim Sönmez Sayili
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    Abstract: Polymetallic mineralizations around Mayıslar Village (Sarıcakaya-Eskişehir) are located in andesiticrocks of Eocene aged Meyildere Volcanites and in ultramafic rocks of Cretaceous aged Dağküplü Melangewhich is tectonically emplaced in the region. The mineralizations are formed at different stages andcaused alterations in the host rocks. Quartz and calcite veins intersect the altered andesites which aresilicified, seriticized, argillized and enriched by tourmalines. According to macroscopic and microscopicinvestigatons, at least two quartz generations as early and late quartzs (Quartz-I and Quartz-II) andcalcite formations together with and further than late stage quartzs have been determined. Ore microscopicstudies have revealed that in addition to oxide and sulfide minerals in the host rocks, sulfide minerals suchas pyrrhotite, pyrite, chalcopyrite, galena, sphalerite, fahlore and arseopyrite are determined.Fluid inclusion studies carried out on quartzs and calcites showed that Quartz-I generation exhibit theformation temperatures of 4700 - 3700 C and salinities of 27- 41% NaCl equivalent. Late stage quartzs(Quartz-II) and accompanying calcites with some exceptions between 3700 - 2700 C, display the formationtemperatures of 2700 -1100 C and salinities under 7% NaCl equivalent. Ore minerals seem to occur withlate stage quarzs and calcites.Considering together of alteration and ore minerals, tourmalines and fluid inclusion data strengthen thepossibility of a buried granitoidic intrusion. All these data indicate the reasonable view of siliceous,carbonaceous and ore bearing solutions moved from this intrusion due to tectonic activities as differentstages altered andesites and other country rocks and caused the formation of mineralizations.

  • Calcite

  • Eskişehir-Mayıslar

  • fluid inclusion

  • polymetallic mineralizations

  • quartz


  • Akıska, S. 2010. Yenice (Çanakkale) Bölgesi’ndeki Cu-Pb-Zn Oluşumları. A.Ü Fen Bilimleri Enst. Doktora Tezi, 234 s. (yayımlanmamış).

  • Bodnar, R.J.,1993. Revised equation and table for determining the freezing point depression of H2O-NaCl solutions. Geochimica et Cosmochimica Acta, 57, 683-684.

  • Bodnar, RJ., 2003. Reequilibration of fluid inclusions: in I.Samson, A.Anderson,&D. Marshall, eds.Fluid Inclusions: Analysis and Interpretation. Mineral. Assoc.Canada, Short Course 32, 213-230.

  • Cavaretta, G. and Puxeddu, M. 1990. Schorl-dravite-ferridravite tourmalines deposited by hydrothermal magmatic fluids early evolution of the Lardello geothermal field, Italy. Economic Geology, 85 no.6, 1236-1251.

  • Coşkun, E., 2010. Akdağmadeni (Yozgat), Pb-Zn Yataklarında Metamorfizma etkisinin Araştırılması. Hacettepe Üniversitesi Fen Bilimleri Enstitüsü., Ankara, Doktora Tezi, 160s. (yayımlanmamış).

  • Delibaş (Coşkun), E., Genç, Y. 2004. Terziali-Çayağzı (Kırşehir) Altın Cevherleşmesi: Kırşehir Masifinde saprolitik altın zenginleşmelerinin ilk bulguları. Yer Bilimleri, 23-33.

  • Demirela, G. 2011. Çataltepe (Lapseki/Çanakkale) Pb-Zn±Cu±Ag Yatağı’nın Jeolojisi ve Kökeni. AÜ Fen Bilimleri Enst. Doktora Tezi, 220 s.(yayımlanmamış).

  • Duru, M., Pehlivan, Ş, Kandemir, Ö., Kanar,F.,Tok, T., Karakaya Kuşağının Jeolojisi ve Jeodinamik Evrimi , MTA Genel Müdürlüğü, (Yayına hazırlanmakta).

  • Gedik, İ. ve Aksay, A. 2002, 1/100000 ölçekli Türkiye Jeoloji Haritaları Adapazarı H 25 paftası, MTA yayınları, Ankara

  • Gleeson, S.A, Wilkinson, J.J., Stuart, F.M. and Banks, D.A. 2001. The origin and evolution of base metal mineralising brines and hydrothermal fluids, South Cornwall, UK. Geochimica et Cosmochimica Acta. V. 65 No. 13, 2067- 2079.

  • Göncüoğlu, M.C., Turhan, N., Şentürk, K., Uysal, Ş., Özcan, A. ve Işık, A., 1996, Orta Sakarya’da Nallıhan-Sarıcakaya arasındaki yapısal birliklerin jeolojik özellikleri: MTA Der. Rap. No. 10094.

  • Güllü, B. ve Kadıoğlu, Y.K. 2012, Turmalinli Kuvars Damarlarının Kökeni: Karakaya (Kaymaz) İntrüzif Kütlesi Eskişehir, Türkiye. Yüzüncü Yıl Üniversitesi Fen Bilimleri Dergisi 17 (1): 20-28, Araştırma Makalesi, Van.

  • Harraz, H.Z. 2000. A genetic model for a mesothermal Au deposit: evidence from fluid inclusions and stable isotopic studies at El Sid Gold Mine, Eastern Desert, Egypt. Journal of African Earth Sciences. Vol. 30 No.2 267-282.

  • Hein, U.F., 1989, Microthermometry, Compact Course and Exercises, IGDL, University of Göttingen, 52s.

  • Heinrich, C.A., Günther, D., Audétat, A. Ulrich, T. and Frischknecht, F., 1999. Metal fractionation between magmatic brine and vapor determined by microanalysis of fluid inclusions. Geology, V.27, 755-758.

  • Heinrich, C.A. 2007. Fluid-Fluid interactions in magmatichydrothermal ore formation. Reviews in Mineralogy and Geochemistry, v.65 No.1 363-387.

  • Kalender, L., Sağiroğlu, A. and Kişman, S. 2009. Fluid inclusion studies in the different origin quartzs associated with CuPb-Zn mineralizations at Kizildag and Köprücük-Harput, East Anatolian District, Turkey. Ozean Journal of Applied Sciences 2 (1), 127-138.

  • Kibici, Y. 1984, Sarıcakaya Masifinin jeolojisi, petrografisi ve petrolojik etüdü: Doktora tezi, Anadolu Üniversitesi Yayınları, 68.

  • Kibici, Y. 1990. Sarıcakaya Volkanitlerinin Petrolojisi ve Kökensel Yorumu. Türkiye Jeoloji Bülteni, C. 33,69-77.

  • Kibici, Y. 1999. Geochemical properties and genetical interpretation of the central Sakarya region granitoid belt. Afyon Kocatepe University, Juornal of Science 1, 143-157.

  • Kibici, Y. İlbeyli, N., Yıldız, A. and Bağcı, M., 2010. Geochemical constraints on the genesis of the Sarıcakaya intrusive rocks, Turkey: Late Paleozoic crustal melting in the central Sakarya Zone. Chemie der Erde 70, 243-256.

  • Lai, J and Chi, G, 2007, CO2-rich fluid inclusions with chalcopyrite daughter mineral from the Fenghuangshan Cu-Fe-Au deposits, China: implicaions for metal transport in vapor, mineral Daposita,42:293-299.

  • Okay, A.İ., 1984, Kuzeybatı Anadolu’da yer alan metamorfik kuşaklar: Ketin Sempozyumu, TJK Yayını .

  • Okay, A.İ., 2004, Türkiye Jeolojisinde paleotetis problemi, 57.TJK Bildiri Özleri Kitabı, 8-10.

  • Parlak, B., Eskişehir -Sarıcakaya Mayıslar Polimetalik Cevher Oluşumlarının Maden Jeolojik İncelemesi , Ankara Üniversitesi Doktora Tezi, hazırlanmakta.

  • Robb, L. 2005, Introduction of ore forming processes. Blackwell Publishing Company. 372pp.

  • Roedder, E., 1984, Fluid inclusions, Min. Soc. Am. Rev. in Min., v.12, 646p.

  • Sawkins, F. J. 1984, Metal Deposits in relation to Plate Tectonics. Minerals and Rocks series, Volume 17. xiv, 325 pp. Berlin, Heidelberg, New York, Tokyo: Springer Verlag.

  • Sawkins, F. J. 1990, Metal Deposits in relation to Plate Tectonics. 2nd. Ed. xix. 461pp. Berlin, Heidelberg, New York, Tokyo: Springer Verlag.

  • Sterner, S.M., Hall, D.L. and Bodnar, R. J., 1988, Synthetic fluid inclusions. V. Solubility relations in the system NaClKCl-H2O under vapor-saturated conditions. Geochimica et Cosmochimica Acta, 52, 989-1006.

  • Sourirajan, S.and Kennedy, G.C., 1962. The system H2 O-NaCl at elevated temperatures and pressures. Am. J. Sci. 260,115- 141.

  • Ustaömer, P.A., Ustaömer, T. and Robertson, A.H.F., 2012. Ion probe U-Pb Dating of the central Sakarya Basement: A periGondwana Terrane intruded by late Lower Carboniferous subduction/collision related granitic rocks. Turkish Journal of Earth Sciences Vol. 21, 905-932.

  • Wilkinson, J.J. 2001. Fluid inclusions in hydrothermal ore deposits. Lithos 55, 229-272.

  • Yıldırım, S., Yıldız, H., Ak, S., Niğdeli, F. ve Turgut, B., 2002, Eskişehir-Sarıcakaya-Mayıslar Altın Cevherleşmesinin (Ön.İr.10415;Erişim No:240 13 67) Buluculuk Talebine Esas Maden jeolojisi ve Rezerv Raporu., MTA Derleme No:11074, Ankara.

  • Yıldırım, B.A., Kalender, L. ve Şaşmaz, A. 2010. Çolaklı (Elazığ) çevresindeki Pb-Zn-Cu cevherleşmeleri ile ilişkili kuvarslarda sıvı kapanım incelemeleri. IV. Ulusal Jeokimya Sempozyumu bildirileri. S 87-88.

  • Zhang, D., Xu, G., Zhang, W. and Golding, S.D. 2007. High salinity fluid inclusions in the Yinshan polymetallic deposit from the Le-De metallogenic belt in Jiangxi Province, China: Their origin and implications for ore genesis. Ore Geology Reviews. V. 31 247-260.

  • Parlak, B , Sayılı, İ . (2012). Mayıslar Sahası (Sarıcakaya-Eskişehir) Polimetal Cevherleşmeleri Alterasyon Zonları İçindeki Kuvars ve Kalsitlerde Sıvı Kapanım Verileri . Türkiye Jeoloji Bülteni , 55 (2) , 111-136 . Retrieved from https://dergipark.org.tr/tr/pub/tjb/issue/28143/299137

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