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Year 2015, Volume: 5 Issue: 1, 34 - 49, 02.02.2015

Kübra Akbulut Enver Akaryalı , İbrahim Akpınar Emre Aydınçakır

https://doi.org/10.17714/gufbed.2015.05.003
Cited By: 2

Abstract

The investigation area in this study covers the immediate surroundings of Eylence Yayla and Emirinkomu, Ünlüpınar (Pekün) Town of Kelkit County located south of Gümüşhane Province. Kurtoğlu Metamorphics, Şenköy Formation and Köse Granitoid are located in the study area. The Zn-Pb-Cu ± Au mineralization located in Eylence Yayla and Emirinkomu sites is completely settled into the N20E striking fault lines within andesites belonging to Şenköy Formation. To reveal the mineralization assemblages in the study area, the polished samples which prepared from systematic samples were examined under the ore microscopy. The paragenesis of the mineralization is determined according to the order of occurrence, as pyrite, chalcopyrite, sphalerite, galena, gold, quartz and calcite. The hematitization, limonitization and sulfurization are identified as alteration types, based on the observations made on the field. According to the results of the fluid inclusion studies, the formation temperature of mineralization changes between 80 and 280C. Based on the sulphur isotope thermometer analysis, the average formation temperature of mineralization is determined as 264C

Keywords

Gold Stable isotope Kelkit Lead-zinc Fluid inclusion

References

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  • Akaryalı, E., 2010. Arzular (Gümüşhane KD-Türkiye) Altın Yatağının Jeolojik, Mineralojik, Jeokimyasal Ve Kökensel İncelenmesi, Doktora Tezi, KTÜ, Fen Bilimleri Enstitüsü, Trabzon.
  • Akaryalı, E., Tüysüz, N., 2013. The genesis of the slab window-related Arzular low-sulfidation epithermal gold mineralization (Eastern Pontides, NE Turkey). Geoscience Frontiers, 4-4,409-421.
  • Akçay, M., Gündüz, Ö. ve Çoban, H., 1998. A Multi-phase Intrusion Around the GümüşhaneVillage (Artvin) and Associated Mineralisation Types: A Geologic and Geochemical Approach, Geosound, 33, 1-18.
  • Aslaner, M., 1977. TürkiyeBakır-kurşun-çinko Yataklarının Jeolojik ve BölgeselSınıflamasıylaPlakaTektoniğiYönünden İncelenmesi, KTÜ YerbilimleriFakültesi, Yayın No: 12, Trabzon.
  • Bacon, C.R. ve Hirschmann, M.M., 1988. Mg/Mn partitioning as a test for equilibrium between coexisting Fe-Ti oxides, American Mineralogist. 73, 57-61.
  • Bakker, R.J., 2003. Package FLUIDS 1. Computer Programs for Analysis of FluidInclusion Data andforModellingBulkFluidProperties, Chem. Geol., 194, 3-23.
  • Barret, T.J. ve MacLean, W.H., 1991. Chemical, Mass, and Oxygen Isotopic Changes During Extreme Hydrothermal Alteration of an Archean Rhyolite, Noranda, Econ. Geology, 86, 406-441.
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  • Kandemir, R., 2004. Gümüşhane ve Yakın Yörelerindeki Erken-Orta Jura Yaşlı Şenköy Formasyonu’nun Çökel Özellikleri ve BirikimKoşulları, DoktoraTezi, Karadeniz Üniversitesi, Fen BilimleriEnstitüsü, Trabzon.
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Ünlüpınar (Kelkit-Gümüşhane) Pb-Zn±Au Cevherleşmesinin Jeolojik, Jeokimyasal ve Kökensel Olarak İncelenmesi

Year 2015, Volume: 5 Issue: 1, 34 - 49, 02.02.2015

Kübra Akbulut Enver Akaryalı , İbrahim Akpınar Emre Aydınçakır

https://doi.org/10.17714/gufbed.2015.05.003
Cited By: 2

Abstract

İnceleme alanı Gümüşhane ilinin güneyinde yer alan Kelkit İlçesi Ünlüpınar (Pekün) Beldesine bağlı Eylence Yayla ve Emirinkomu Köyü yakın çevresi kapsamaktadır. Bu çalışmada bölgenin 1/25.000 ölçekli jeolojik harita ve cevherleşmenin içinde yer aldığı sahaların 1/5.000 ölçekli detay maden jeoloji haritası yapılmıştır. Çalışma alanında Kurtoğlu Metamorfikleri, Şenköy Formasyonu ve Köse Granitoyidi yer almaktadır. Liyas yaşlı volkanik kayaçların sınıflandırılmasında, hareketsiz elementler kullanılarak oluşturulan Nb/Y-Zr/TiO2 diyagramı ile Şenköy Formasyonu’ndan alınan örneklerin andezit-bazalt ve andezit sınırında toplandığı görülmüştür. Liyas volkanik kayaçları plajiyoklas, klinopiroksen ve Fe-Ti oksit minerallerini içermektedir. Yapılan mineral kimyası analizleri sonucunda plajiyoklasların bitovnit(An73-78), labrador (An51-64)  ve andezin (An32-42) bileşiminde olduğu, klinoproksenlerin ojit ve klinoenstatit (Wo33.418-39.358 En 38.565-61.792 Fs18.220-27.230) bileşiminde olduğu,  Fe-Ti oksitlerin ise titano-magnetitbileşiminde olduğu belirlenmiştir. Detay inceleme yapılan alan ve yakın çevresindeki birim Erken-Orta Jura yaşlı Şenköy Formasyonu'na ait bazalt, bazaltik andezit ve piroklastları oluşturmaktadır. Eylence Yaylave Emirinkomu mevkiinde yer alan Zn-Pb-Cu ± Au cevherleşmesi tamamen Şenköy Formasyonuna ait bazaltik andezitler içinde K20D doğrultularındaki kırık hatlarına yerleşmiştir. İnceleme alanında cevherleşmenin parajenezini ortaya çıkarmak içinde çalışma sahasından sistematik örneklerden parlak kesitler yapılarak, cevher mikroskobisi altında incelenmiştir. Cevherleşmenin parajenezi oluşum sırasına göre pirit, kalkopirit, sfalerit, galen, altın, kuvars ve kalsit olarak tespit edilmiştir.Arazide yapılan gözlemler sonucunda alterasyon türleri olarak hematitleşme, limonitleşme ve kükürtleşme tespit edilmiştir. Sıvı kapanım analiz sonuçlarına göre cevherleşmenin oluşum sıcaklığının 80-2800C arasında değiştiği, kükürt izotop termometresine göre ise cevherleşmenin oluşum sıcaklığının ortalama 2640C olduğu belirlenmiştir.

Keywords

Altın; Duraylı izotop; Kelkit; Kurşun-Çinko; Sıvı kapanım

References

  • Adamia, S., Lordkitanidze, M.B. ve Zakariadze, G.S., 1977. Evoluation of an Active Continental Margine as Examplified by the Alpine History of Caucasus, Tectonophysics, 40, 183-189.
  • Akaryalı, E., 2010. Arzular (Gümüşhane KD-Türkiye) Altın Yatağının Jeolojik, Mineralojik, Jeokimyasal Ve Kökensel İncelenmesi, Doktora Tezi, KTÜ, Fen Bilimleri Enstitüsü, Trabzon.
  • Akaryalı, E., Tüysüz, N., 2013. The genesis of the slab window-related Arzular low-sulfidation epithermal gold mineralization (Eastern Pontides, NE Turkey). Geoscience Frontiers, 4-4,409-421.
  • Akçay, M., Gündüz, Ö. ve Çoban, H., 1998. A Multi-phase Intrusion Around the GümüşhaneVillage (Artvin) and Associated Mineralisation Types: A Geologic and Geochemical Approach, Geosound, 33, 1-18.
  • Aslaner, M., 1977. TürkiyeBakır-kurşun-çinko Yataklarının Jeolojik ve BölgeselSınıflamasıylaPlakaTektoniğiYönünden İncelenmesi, KTÜ YerbilimleriFakültesi, Yayın No: 12, Trabzon.
  • Bacon, C.R. ve Hirschmann, M.M., 1988. Mg/Mn partitioning as a test for equilibrium between coexisting Fe-Ti oxides, American Mineralogist. 73, 57-61.
  • Bakker, R.J., 2003. Package FLUIDS 1. Computer Programs for Analysis of FluidInclusion Data andforModellingBulkFluidProperties, Chem. Geol., 194, 3-23.
  • Barret, T.J. ve MacLean, W.H., 1991. Chemical, Mass, and Oxygen Isotopic Changes During Extreme Hydrothermal Alteration of an Archean Rhyolite, Noranda, Econ. Geology, 86, 406-441.
  • Barret, T.J., Cattalani, S. ve MacLean, W.H., 1991a. Massive Sulfide Deposits of the Noranda Area, Quebec. I. The Horne Mine, Can. J. Earth Sci., 28, 465-488.
  • Barret, T.J., Cattalani, S., Chartrand, F. ve Jones, P., 1991b. Massive Sulfide Deposits of the Noranda Area, Quebec. II. The Aldermac Mine, Can. J. Earth Sci., 28, 1301-1327.
  • Barret, T.J., MacLean, W.H., Cattalani, S., Hoy, L. ve Riverin, G., 1991c. Massive Sulfide Deposits of the Noranda Area, Quebec. III. The Ansil Mine, Can. J. Earth Sci., 28, 1699-1733.
  • Barret, T.J. Cattalani, S. and Maclean W.H., 1993. Volcanic lithogeochemistry and alteration at the Delbridge massive sulfide deposit, Noranda Quebec, Jour. Of Geochem. Expoloration, 48, 135-173
  • Bektaş, O. ve Güven, İ.H., 1995. Alaskan Aphinitic Type Ultramafic and Mafic Complexes as the Root Zone of the Eastern Pontide Magmatic Arc (NE Turkey), Geology of the Black Sea Region, 189-196. Ankara.
  • Bodnar, R.J., 1993. Revised Equation and Table for Determining the Freezing Point Depression of H2O-NaCl Solutions, Geochim. Cosmochim. Acta, 57, 683-684.
  • Boynton, W. V., 1984. Cosmochemistry of Rare Earth Elements: MeteoriteStudies. In: Henderson, P. (Ed), Rare Earth Element Geochemistry, Elsevier, Amsterdam., 63-114.
  • Brown, P.E., 1989. Flinkor: A Microcomputer Program fortheReductionandInvestigation of Fluid-Inclusion Data, Am. Mineral., 74, 1390-1393.
  • Campbell, A:R. ve Larson,P.B., 1998. Introductiontostableisotopeapplications in hydrothermalsystems, in Richhards, P.J., Larson, J.P., eds., Techniques in HydrothermalOreDepositsGeology, Reviews in Econ. Geology, 10, 173-193.
  • Cooke, D.R. ve Simmons, S.F., 2000. Characteristics and Genesis of Epithermal Gold Deposit. In Hageman, G.S., Brown, E. (eds), Gold in 2000, reveiwsinEconomic Geology, 13, 221-241.
  • Çiftçi, E., 2000. Mineralogy, Paragenetic Sequence, Geochemistry and Genesis of the Gold and Silver Bearing Upper Cretaceous Mineral Deposits, North eastern Turkey, Ph. D Thesis, University of Missouri-Rolla, Missouri.
  • Demir, Y., 2005. Istala ve Köstere (Zigana/Gümüşhane) Cu-Pb-Zn Madenleri ve Yan KayaçlarınınMineralojisi ve Dokusal ÖzelliklerininKarşılaştırılmalı İncelenmesi, YüksekLisansTezi, K.T.Ü., Fen BilimleriEnstitüsü, Trabzon.
  • Dixon, J.C. ve Pereire, J., 1974. Plate Tectonics and Mineralization in the Tethyan Region, Min. Deposita, 9, 185-198.
  • Droop, G.T.R. (1987) A general equationforestimating Fe3+ concentration in ferromagnesiansilicatesandoxidesfrommicroprobeanalyses, usingstoichiometriccriteria. Min. Mag, 51, 431-435
  • Erguvanlı, K., 1952. Trabzon-Gümüşhane Arasının Jeolojisi, MTA, Ankara.
  • Eyüboğlu, Y., 2010. Late Cretaceous High-K Volcanism in the Eastern Pontide Orogenic Belt: Implications for the Geodynamic Evolution of NE Turkey, International Geology Review, 52, 142-186.
  • Faure, G., 1986. Principles of Isotope Geology, Second Edition, John Wiley and Sons Inc., New York, 598 s.
  • Field, C.W. ve Fifarek, R.H., 1985. LightIsotopeSytematics in theEpithermal Environment, in Berger, B.R., Bekte, P.M., Eds., GeologyAndGeochemistry of GeothermalSystems, Reviews in Econ. Geology, 2, 99-128.
  • Gettinger, T.E., 1962. 1/500000 ÖlçekliTürkiye Jeoloji Haritası Trabzon Paftası ve İzahnamesi, MTA Yayını, Ankara,
  • Hedenquist, J.W., Matsuhisa, Y., Izawa, E., White, N.C., Giggenbach, W. F. veAoki, M., 1994. Geology, Geochemistry, andOrigin of High Sulfidation Cu-Au Mineralization in theNansatsuDistrict, Japan: EconomicGeology, 89, 1-30.
  • Hoefs, J., 1987. StableIsotopeGeochamistry, 3rd edn. Springer, Berlin-Heidelberg-New York, 241 s.
  • Irvine, T.N. ve Baragar, W.R.A., 1971. A Guide to Chemical Classification of the Common Volcanic Rocks, Can J. Earth. Sci., 8, 523-548.
  • Kandemir, R., 2004. Gümüşhane ve Yakın Yörelerindeki Erken-Orta Jura Yaşlı Şenköy Formasyonu’nun Çökel Özellikleri ve BirikimKoşulları, DoktoraTezi, Karadeniz Üniversitesi, Fen BilimleriEnstitüsü, Trabzon.
  • Le Maitre, R.W., Bateman, P., Dudek, A., Keller, J., Lameyre Le Bas, M.J., Sabine, P.A., Schimid, R., Sorenson, H., Streckeisen, A., Woolley, A.R. ve Zanettin, B., 1989. A Classification of Igneous Rocks and Glossary of Terms Blackwell, Oxford.
  • Leitch, C.H.B., 1981. Mineralogy and Textures of the Lahanos and Kızılkaya Massive Sulfide Deposits, Northeasthern Turkey, and their Similarity to Kuroko Ores, Min. Deposita, 16, 241-257.
  • Lermi, A., 1996. Kanköy (Yomra-Trabzon) CevherindeToprak-BitkiJeokimyasınınUygulanması ve İndikatörBitkiTürüTespiti, YüksekLisansTezi, K.T.Ü., Fen BilimleriEnstitüsü, Trabzon.
  • Lermi, A., 2003. Midi (Karamustafa/Gümüşhane, KD Türkiye) Zn-Pb Yatağının Jeolojik, Mineralojik, Jeokimyasal ve Kökensel İncelemesi, DoktoraTezi, K.T.Ü., Fen BilimleriEnstitüsü, Trabzon.
  • MacLean, W.H. ve Kranidiotis, P., 1987. Immobile Elements as Monitors of Mass Transfer in Hydrothermal Alteration: Phelps Dogge Massive Sulfide Deposit, Matagami, Quebec, Econ. Geology, 82, 951-962.
  • MacLean, W.H., 1990. Mass Change Calculations in Altered Rock Series, Mineral Deposita, 25, 44-49.
  • Meschede, M., 1986. A method of discriminating between different types of mid-ocean ridge basalts and continental tholeiites with the Nb-Zr-Y diagram, Chemical Geology, 56, 207-218.
  • Morimoto, M., 1988. Nomenclature pyroxenes, Mineralogical Magasine, 52, 535-550.
  • O'Neil, J. R., 1986. Theoretical and Experimental Aspects of Isotopic Fractionation, In: Valley, W. and J. R. O'Neil (Eds.), Stable Isotopes in High Temperatures Geological Processes, Reviews in Mineralogy, 16, 1-40.
  • Ohmoto, H., 1986. Stable Isotope Geochemistry of Ore Deposits: In Valley, J. W., Taylor, H. P. And O'Nein, J. R. (eds.), Stable Isotopes in High Temperature Geological Processes, Reviews in Mineralogy, Mineralogical Society of America, 16, 491 -560.
  • Ohmoto, H. ve Rye R.O., 1970. TheBluebell Mine, British Colombia. I. Minerology, Paragenesis, Fluidİnclusionsandtheİsotops of HydrogenOxygenandCarbon, Econ. Geology, 65, 417-437.
  • Pearce, J.A., Cann, J. R., 1973. Tectonic setting of basic volcanic rocks determined using trace element analyses, Earth Planett. Sci. Lett., 19, 290-300.
  • Pearce, J.A., 1996. A User’s Guide to Basalt Discrimination Diagrams, in Wyman, D.A., ed., Trace Element Geochemistry of Volcanic Rocks: Applications for Massive Sulphide Exploration, Geological Association of Canada, Short Course Notes, 12, 79-113.
  • Potter, R.W., Clynne M.A. ve Brown D.L. 1978. Freezing Point Depression of AqueousSodiumChloride Solutions, Econ. Geol., 73, 284-285.
  • Roedder, E., 1984. Fluid Inclusions: Reviews in Minorology, v. 12, Mineralogical Society of America, Washington, 644.
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Details

Primary Language Turkish
Journal Section Articles
Authors

Kübra Akbulut This is me

Enver Akaryalı

İbrahim Akpınar This is me

Emre Aydınçakır

Publication Date February 2, 2015
Submission Date September 29, 2014
Published in Issue Year 2015 Volume: 5 Issue: 1

Cite

APA Akbulut, K., Akaryalı, E., Akpınar, İ., Aydınçakır, E. (2015). Ünlüpınar (Kelkit-Gümüşhane) Pb-Zn±Au Cevherleşmesinin Jeolojik, Jeokimyasal ve Kökensel Olarak İncelenmesi. Gümüşhane Üniversitesi Fen Bilimleri Dergisi, 5(1), 34-49. https://doi.org/10.17714/gufbed.2015.05.003

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