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Sarıcakaya (Eskişehir) Granitoyidindeki Pegmatitlerin Kökeni ve Endüstriyel Hammadde Potansiyeli

Yıl 2023, Cilt: 5 Sayı: 2, 371 - 382, 27.10.2023
https://doi.org/10.46387/bjesr.1347030

Öz

Eskişehir kuzeyindeki Sarıcakaya Granitoidindeki pegmatitlerin ana mineralojik bileşeni plajiyoklaz, ortoklaz, kuvars, biyotit, ±granat, ±muskovit, ±epidot’tur. Konfokal raman spektroskopi çalışmalarında plajiyoklaz minerallerinin albit-oligoklaz, granatların ise çoğunlukla spessartin bileşimde oldukları görülmektedir. Endüstriyel hammadde olarak kullanılabilme potansiyeline sahip pegmatitler ana kaya ile keskin dokanaklı olup, serizitleşme ve killeşme gösterirler.
Pegmatitlerin A/NK (mol%) oranı 0.96-1,79 (ortalama 1,32), A/CNK (mol%) oranları 0.82-1.55 (ortalama:1,07) arasında değişmekte olup metalümin-peralümin karakteri yansıtmaktadır. Zirkon ve apatit doygunluk sıcaklıkları pegmatitleri oluşturan magmanın ortalama sıcaklığının 678,7-766,7°C aralığında değiştiğini göstermektedir. ORG’ye göre normalize edilen örümcek diyagramlarda kabuksal kirlenmenin etkilerinin gözlendiği pegmatitlerin, Sarıcakaya granitoidini oluşturan magmanın pegmatitik-pnömatolitik evredeki kristallenen magmatik birimleri olduğu düşünülmektedir.

Destekleyen Kurum

AKSARAY ÜNİVERSİTESİ Bilimsel Araştırma Projeleri Komisyonu

Proje Numarası

BAP-2015-077

Teşekkür

Bu çalışma AKSARAY ÜNİVERSİTESİ Bilimsel Araştırma Projeleri Komisyonu tarafından BAP-2015-077 no’lu proje ile desteklenmiştir. Yazarlar katkılarından dolayı Aksaray Üniversitesine ve çalışmanın laboratuvar kritik aşamalarındaki katkılarından dolayı Ankara Üniversitesi Yer Bilimleri Uygulama ve Araştırma Merkezi (YEBİM) yöneticisi Doç. Dr. Kıymet DENİZ YAĞCIOĞLU’na teşekkür ederler.

Kaynakça

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  • H.G. Dill “Pegmatites and aplites: Their Genetic and Applied Ore Geology”, Ore Geol Rev, vol. 69, pp. 417-561, 2015.
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  • Y. Marzoni Fecia Di Cossato, P. Orlandi, and G. Vezzalini “Rittmannite, A New Mineral Species of the Whiteite Group from the Mangualde Granitic Pegmatite, Portugal”, Can Mineral, vol. 27, pp. 447–449, 1989.
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  • W.D. Birch, A. Pring, and E.E. Foord “Selwynite, Nak(Be, Al)Zr2(PO4)4 2H2O, A New Gainesite-Like Mineral from Wycheproof, Victoria, Australia”, Can Mineral, vol. 33, pp.55-58, 1995.
  • W.D. Birch, I.E. Grey, S.J. Mills, A. Pring, C. Bougero, A. Ribaldi-Tunnicliffe, N.C. Wilson, and E. Keck “Nordgauite, MnAl2(PO4)2(F,OH)2. 5H2O, A New Mineral from the Hagendorf–Süd Pegmatite, Bavaria, Germany: Description and Crystal Structure”, Mineral Mag, vol. 75, pp. 269–278, 2011.
  • G. Adiwidjana, K. Friese, K.H. Klaska, and J. Schlüter “The Crystal Structure of Kastningite (Mn, Fe, Mg)(H2O)4[Al2(OH)2(H2O)2(PO4)2]⋅2H2O - A New Hydroxyl Aquated Orthophosphate Hydrate Mineral”, Z. Kristallogr, vol. 214, pp. 465–468,1999.
  • G. Raade, G. Ferraris, A. Gula, G. Ivaldi, and F. Bernhard “Kristianesite A New Calcium-Scandium-Tin Sorosilicate from Granite Pegmatite from Tørdal, Telemark, Norway”, Mineral Petrol, vol. 75, pp. 89–99, 2002.
  • J. Brugger, N. Meisser, B. Etschmann, S. Ansermet, andA. Pring “Paulscherrerite From The Number 2 Workings, Mount Painter Inlier, Northern Flinders Ranges, South Australia; “Dehydrated Schoepite” is a Mineral After All”, Am Mineral, vol. 96, pp.229–240, 2011.
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  • J. Oyarzábal, M.Á. Galliski, and E. Perino “Geochemistry of K-Feldspar and Muscovite in Rare-Element Pegmatites and Granites from the Totoral Pegmatite Field, San Luis, Argentina”, Resour Geol, vol. 59, pp. 315–329, 2009.
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Nature and Industrial Raw Material Potential of Pegmatites within the Sarıcakaya (Eskişehir) Granitoid

Yıl 2023, Cilt: 5 Sayı: 2, 371 - 382, 27.10.2023
https://doi.org/10.46387/bjesr.1347030

Öz

The main mineralogical component of the pegmatites in the Sarıcakaya Granitoid in the north of Eskişehir are plagioclase + orthoclase + quartz + biotite ± garnet ± muscovite ± epidote. According to Confocal Raman Spectroscopy studies, plagioclase minerals are albite-oligoclase, and garnets are mostly in spessartine composition. Pegmatites, which have the potential to be usable as industrial raw materials, are in sharp contact with the hostrock and show sericitization and argillization. The A/NK (mol%) ratio of pegmatites ranges from 0.96-1.79 (avr. 1.32), A/CNK (mol%) ratios range between 0.82-1.55 (avr. 1.07), reflecting the metalumin to peralumin character. Zircon and apatite saturation temperatures show that the average temperature of the magma forming the pegmatites varies in the range of 678.7-766.7°C. The pegmatites, in which the effects of crustal contamination are observed in the spider diagrams normalized according to ORG, are thought to be the crystallized magmatic units of the magma forming the Sarıcakaya granitoid in the pegmatitic-pneumatolytic phase.

Proje Numarası

BAP-2015-077

Kaynakça

  • R.L. Linnen, M. Van Lichtervelde, and P.Černý “Granitic Pegmatites as Sources of Strategic Metals”, Elements, vol. 8, pp. 275-280, 2012.
  • H.G. Dill “Pegmatites and aplites: Their Genetic and Applied Ore Geology”, Ore Geol Rev, vol. 69, pp. 417-561, 2015.
  • H. Strunz, “Laueit,MnFe2 3+[OH|PO4]2·8H2O, ein neues mineral”, Naturwissenschaften, vol 41, 256p, 1954a.
  • H. Strunz “Hagendorfit, ein neues Mineral der Varulith-Hühnerkobelit-Reihe”, Neues Jb Mineral Monat, pp. 252–255, 1954b.
  • H. Schneiderhöhn “Die Pegmatite (The pegmatites)”, Gustav Fischer Verlag, Stuttgart, 720 p. 1961.
  • E. Seeliger, and A. Mücke “Ernstit, ein neues Mn2+Fe3+ - Phosphat und seine Beziehungen zum Eosphorit”, Neues Jb Mineral Monat, pp. 289-298, 1970.
  • P.B. Moore, and A.R. Kampf “Schoonerite, A New Zinc-Manganese-Iron Phosphate Mineral”, Am Mineral, vol. 62, pp 246–249, 1977.
  • B.D. Sturman, R.C. Rouse and, P.J. Dunn “Parascholzite, A New Mineral from Hagendorf, Bavaria, And Its Relationship to Scholzite”, Am Mineral, vol. 66, pp. 843–851, 1981.
  • Y. Marzoni Fecia Di Cossato, P. Orlandi, and G. Vezzalini “Rittmannite, A New Mineral Species of the Whiteite Group from the Mangualde Granitic Pegmatite, Portugal”, Can Mineral, vol. 27, pp. 447–449, 1989.
  • F. Walter, W. Postl, and J. Taucher “Weinebeneit: Paragenese und Morphologie eines neuen Ca–Be-Phosphates von de r Spodumenpegmatit-Lagerstätte Weinebene,Koralpe, Kärnten”, Mitt Abt Mineral, Landesmuseum Joanneum, vol. 58, pp.37–43, 1990.
  • W.D. Birch, A. Pring, and E.E. Foord “Selwynite, Nak(Be, Al)Zr2(PO4)4 2H2O, A New Gainesite-Like Mineral from Wycheproof, Victoria, Australia”, Can Mineral, vol. 33, pp.55-58, 1995.
  • W.D. Birch, I.E. Grey, S.J. Mills, A. Pring, C. Bougero, A. Ribaldi-Tunnicliffe, N.C. Wilson, and E. Keck “Nordgauite, MnAl2(PO4)2(F,OH)2. 5H2O, A New Mineral from the Hagendorf–Süd Pegmatite, Bavaria, Germany: Description and Crystal Structure”, Mineral Mag, vol. 75, pp. 269–278, 2011.
  • G. Adiwidjana, K. Friese, K.H. Klaska, and J. Schlüter “The Crystal Structure of Kastningite (Mn, Fe, Mg)(H2O)4[Al2(OH)2(H2O)2(PO4)2]⋅2H2O - A New Hydroxyl Aquated Orthophosphate Hydrate Mineral”, Z. Kristallogr, vol. 214, pp. 465–468,1999.
  • G. Raade, G. Ferraris, A. Gula, G. Ivaldi, and F. Bernhard “Kristianesite A New Calcium-Scandium-Tin Sorosilicate from Granite Pegmatite from Tørdal, Telemark, Norway”, Mineral Petrol, vol. 75, pp. 89–99, 2002.
  • J. Brugger, N. Meisser, B. Etschmann, S. Ansermet, andA. Pring “Paulscherrerite From The Number 2 Workings, Mount Painter Inlier, Northern Flinders Ranges, South Australia; “Dehydrated Schoepite” is a Mineral After All”, Am Mineral, vol. 96, pp.229–240, 2011.
  • V.N. Yakovenchuk, E. Keck, S.V. Krivovichev, Y.A. Pakhomovsky, E.A. Selivanova, J.A. Mikhailova, A.P. Chernyatieva, G.Y. Ivanyuk “Whiteite-(Camnmn), CaMnMn2Al2[PO4]4(OH)2∗8H2O, “A New Mineral From The Hagendorf-Süd Granitic Pegmatite, Germany”, Mineral Mag, vol. 76, pp. 2761–2771, 2012.
  • T. Koralay, Y.K. Kadıoglu, and S.Y. Jiang “Determination of Tourmaline Composition in Pegmatite From Buldan, Denizli (Western Anatolia, Turkey) Using XRD, XRF, and Confocal Raman Spectroscopy”, Spectrosc Lett, vol. 46, pp. 499-506, 2013.
  • P. Černy “Geochemical and Petrogenetic Features of Mineralization in Rare-Element Granitic Pegmatites in The Light of Current Research”, Appl Geochem, vol. 7, pp.393–416, 1992.
  • M.A. Wise, and P. Černý “The Crystal Chemistry of the Tapiolite Series”, Can Mineral, vol. 34, pp.631–647, 1996.
  • R.J. Bakker, and M.A. Elburg “Amagmatic–Hydrothermal Transition in Arkaroola (Northern Flinders Ranges, South Australia); from Diopside-Titanite Pegmatites to Hematite-Quartz Growth”, Contrib Mineral Petrol, vol. 152, pp. 541–569, 2006.
  • J. Oyarzábal, M.Á. Galliski, and E. Perino “Geochemistry of K-Feldspar and Muscovite in Rare-Element Pegmatites and Granites from the Totoral Pegmatite Field, San Luis, Argentina”, Resour Geol, vol. 59, pp. 315–329, 2009.
  • R. Thomas, and P. Davidson “The Missing Link between Granites and Granitic Pegmatites”, J Geosci, vol. 58, pp.183-200, 2013.
  • P. Černý, P.L. Blevin, M. Cuney, and D. London “Granite-Related Ore Deposits”, Econ Geol,100th Anniversary Volume, pp. 337-370, 2005.
  • P. Černý, and S. Ercit “The Classification of Granitic Pegmatites Revisited”, Can Mineral, vol. 43, pp. 2005–2026, 2005.
  • D. London “Pegmatites”, The Canadian Mineralogist, Special Publication p. 347, 2008.
  • P. Černý “Exploration strategy and methods for pegmatite deposits of tantalum”, In Lanthanides, Tantalum and Niobium (P. Möller, P. Cerny and F. Saupe, eds.), Springer-Verlag, Berlin, pp. 271-299, 1989.
  • D. London “Geochemistry of Alkali and Alkaline Earth Elements in Ore-Forming Granites, Pegmatites And Rhyolites” In: Linnen, R.L., Samson, I. M. (Eds.), Rare Element Geochemistry and Mineral Deposits, Geological Association of Canada Short Course Notes, vol. 17, pp. 17-43, 2005.
  • C. Karaguzel, I. Gulgonul, C. Demir, M. Cinar, and M.S. Celik “Concentration of K-Feldspar from a Pegmatitic Feldspar Ore by Flotation”, Int J Miner Process, vol. 81, pp. 122-132, 2006.
  • M. Melcher, T. Graupner, F. Henjes-Kunst, T. Oberthür, M. Sitnikova, E. Gäbler, A. Gerdes, H. Brätz, D. Davis, and S. Dewaele “Analytical Fingerprint of Columbite– Tantalite (Coltan) Mineralization in Pegmatites: Focus on Africa”, Proceedings, Ninth International Congress for Applied Mineralogy (ICAM), Brisbane, Qld. Australasian Institute of Mining and Metallurgy, pp. 615–624, 2008.
  • D. London, and D.J. Kontak “Granitic Pegmatites: Scientific Wonders and Economic Bonanzas”, Elements, vol. 8, no. 4, pp. 257-261, 2012.
  • Y. Kibici, and G. Güneş “Sivrihisar - Günyüzü (Eskişehir) - Dinek Granitporfırleri İçindeki Feldspatların Ekonomik Potansiyeli”, Endüstriyel Hammaddeler Sempozyumu, İzmir, pp. 83-95, 1995.
  • S. Saklar, C. Oktay, M. Karadeniz, and S. Gürsu “Feldspar Beneficiation from Manisa Alaşehir Pegmatites” International Mining Congress and Exhibition of Turkey-IMCET, pp. 457-459, 2003.
  • I. Bayraktar, S. Ersayın, and Ö.Y Gülsoy “Upgrading Titanium Bearing Na-Feldspar by Flotation Using Sulphonates, Succinamate and Soaps of Vegetable Oils”, Minerals Engineering, vol. 1, no. 12, pp. 1363-1374, 1997.
  • I. Bayraktar, S, Ersayın, and Ö.Y Gülsoy “Magnetic Separation and Flotation of Albite Ore”. In S. Atak, G. Önal, M.S. Celik (Eds.), Innovations in Mineral and Coal Processing, Balkema, Rooterdam, pp. 315-318, 1998.
  • M.S. Çelik, B. Pehlivanoglu, A. Aslanbaş, and R. Asmatulu “Flotation of Colored Impurities from Feldspar Ores”, Minerals and Metallurgical Processing, vol. 18, no. 2, pp. 101-105, 2001.
  • N.T. Selli, and A. Tunalı “Alternatif Hammadde Olarak Pegmatitin Sırlı Porselen Karo Ve Yer Karosu Massesinde Kullanılması”, AKÜ FEMÜBİD, vol. 14, no. OZ5787, pp. 549-552, 2014.
  • O. Bayramgil “Gördes Pegmatitlerinin Mineralojik Etüdü”, Türkiye Jeoloji Bülteni, vol. 5, no. 12, pp. 54-70, 1954.
  • N. Dağ, and Ö. Dora “Gördes (Menderes Masifi Kuzeyi) Pegmadoidleri”, TJK Bülteni, vol. 34, pp. 1-8, 1991.
  • B. Güllü, Y.K. Kadıoğlu, C.Ö. Kılıç, H. Canbaş, K. Deniz, and T. Koralay “Sarıcakaya Granitoyidi İçerisinde Yer Alan Pegmatitlerin Petrokimyasal Karakteristikleri”, Uluslararası Katılımlı VI. Ulusal Jeokimya Sempozyumu Bildiri Özleri Kitabı, pp. 106-108, 2014.
  • H. Bilgilioğlu “Sarıcakaya (Eskişehir) Magmatik Kompleksinin Petrolojik İncelenmesi”, Aksaray Üniversitesi Fen Bil Ens, Doktora Tezi (yayımlanmamış), p. 163, 2019.
  • A.I. Okay “The Geology of the Ağvanis Metamorphic Rocks and Neighbouring Formations”, Bull of the Min Res and Exp, vol. 99, pp. 16-36, 1984a.
  • A.I. Okay “Distribution and Characteristics of The Northwest Turkish Blueschists”, In: J.E. Dixon, and A.H.F. Robertson (Editors), “The Geological Evolution of the Eastern Mediterranean”, Geol. Soc. London Spec. Publ., vol. 17, pp. 455-466, 1984b.
  • I.E. Altınlı “Geology of central Sakarya”, 50th Anniversary of the Republic, Earth Sciences Congress, Ankara, pp. 159-190, 1973.
  • Y. Yılmaz “Tectonic evolution of the southern margin of the Sakarya continent, NW Turkey”, İstanbul Earth Sciences Review, vol. 1, no. 2, pp. 33-51, 1981.
  • C. Demirkol “Üzümlü-Tuzaklı (Bilecik) Dolayının Jeolojisi”, Türkiye Jeoloji Kurumu Bülteni, vol. 20, no.1, Ankara, 1977.
  • B. Güllü, Y.K. Kadıoğlu, T. Koralay, and K. Deniz “Raman Characteristics of Gücünkaya (Aksaray) Gabbroic Rocks, Central Anatolia-Turkey”, 19th International Multidisciplinary Scientific GeoConference SGEM, Bulgaria, vol. 19, pp. 475-482, 2019.
  • M.A. Akçe, and Y.K. Kadıoğlu “Principles of Raman Spectroscopy and Their Uses in the Determination of the Minerals”, Nevşehir Journal of Science and Technology, vol. 9, no.2, pp. 99-115, 2020.
  • K.G. Cox, J.D. Bell, and R.J. Pankhurst “In: The Interpretation of Igneous Rocks”, George Allen & Unwin, London, pp. 450, 1979.
  • T.N. Irvine, and W.R.A. Baragar “A Guide to the Chemical Classification of the Common Volcanick Rocks”, Can J Earth Sci, vol. 8, pp. 523-548, 1971.
  • P.O. Maniar, and P.M. Piccoli “Tectonic Discrimination of Granitoids”, Geological Society of America Bulletin, vol. 101, pp. 635-643, 1989.
  • E.A.K. Middlemost “The Basalt Clan”, Earth-Science Rev, vol. 11, pp. 337-364, 1975.
  • P.C., Rickwood “Boundary Lines Within Petrologic Diagrams Which Use Oxides of Major and Minor Elements”, Lithos, vol. 22, pp. 247-263, 1989.
  • X.H. Li, H.W. Zhou, Y. Liu, C.Y. Lee, M. Sun, and C.H. Chen “Shoshonitic Intrusive Suite in SE Guangxi: Petrology and Geochemistry”. Chinese Science Bulletin, vol. 45, pp. 653-659, 2000.
  • R.R. Meshram, B. Singh, M.K. Mishra, H. Hrushikesh, A. Siddiqui, D. Shukla, R. Akhtar, and T.M. Meshram “Petrological and Geochemical Studies of Lepidolite (LCT Type) and Non-Lepidolite Pegmatite’s from Chakrasila, Dhubri District, Assam, No rth East India”, Open Journal of Geology, vol. 11, pp. 81-104, 2021.
  • J.A. Pearce N.B.W. Harris, and A.G. Tindle, “Trace Element Discrimination Diagrams for the Tectonic Interpratation of Granitic Rocks”, J Petrology, vol. 25, pp. 956-983, 1984.
  • N.M. Evensen, P.J. Hamilton, and R.K. O'Nions “Rare Earth Abundances In Chondritic Meteorites”, Geochimica et Cosmochimica Acta, vol. 42(8), pp. 1199-1212, 1978.
  • W.F. McDonough, and S.S. Sun “The Composition of the Earth”, Chem Geol, vol. 120, pp. 223–253, 1995.
  • T. Koralay, K. Deniz, B. Duman, and Y.K. Kadıoğlu “Mineralogical and Geochemical Characterization and Implications for Provenance of Roman Granite Columns in Ancient Tripolis (Denizli, Turkey)”, Arabian Journal of Geosciences, vol. 14, no. 420, pp. 1-23, 2021.
  • A.M. El Bouseily, and A.A. El Sokkary “The Relation Between Rb, Ba and Sr in Granitic Rocks”, Chemical Geology, vol. 16, pp. 207-219, 1975.
  • M.A. Mckeough, D.R. Lentz, C.R. Mcfarlane, and J. Brown “Geology and Evolution of Pegmatite-Hosted U-Th ± REE-Y-Nb Mineralization, Kulyk, Eagle, and Karin Lakes Region, Wollaston Domain, Northern Saskatchewan, Canada: Examples of the Dual Role of Extreme Fractionation and Hybridization Processes”, Jour of Geosciences, vol. 58, pp. 321-346, 2013.
  • E.B. Watson, and T.M. Harrison “Zircon saturation revisited: temperature and composition effects in a variety of crustal magma types”, Earth and Planetary Science Letters vol. 64, pp. 295-304, 1983.
  • T. M. Harrison, and E. B. Watson “The Behaviour of Apatite During Crustal Anatexis: Equilibrium and Kinetic Considerations”, Geochimica et Cosmochimica Acta, vol. 48, pp. 1467-1477, 1984.
  • B. Güllü, and Y.K. Kadıoğlu “Magmatic Signature of the Closure of the Northern Branch of the Neo-Tethys: Upper Paleocene-Middle Eocene Magmatism At The Boundary Of The Tavşanli-Sakarya Zone (Turkey)”, Geological Quarterly, vol. 66 (13), no. 2, pp. 1-20, 2022.
  • K. Deniz, and Y.K. Kadıoğlu “Investigation of Feldspar Raw Material Potential of Alkali Feldspar Granites and Alkali Feldspar Syenites Within Central Anatolia”, Bulletin of the Mineral Research and Exploration, vol. 158, pp. 265-289, 2019.
  • TS11325, Türk Standartları, 1994, Feldispat Seramik Sanayinde Kullanılan, TSE, Ankara.
  • E. Lewicka “Conditions of the Feldspathic Raw Materials Supply From Domestic and Foreign Sources in Poland”, Gospodarka Surowcami Mineralnymi, vol. 26, no. 4, pp. 5–18, 2010.
  • K. Deniz, and Y.K. Kadıoğlu “Nefelin Siyenitlerin Seramik Sanayiinde Kullanılma Potansiyeli: Buzlukdağ Örneği”, Pamukkale Üniversitesi Mühendislik Bilimleri Dergisi, vol. 24, no. 6, pp. 1209-1219, 2018.
Toplam 67 adet kaynakça vardır.

Ayrıntılar

Birincil Dil Türkçe
Konular Hesaplama Teorisi (Diğer)
Bölüm Araştırma Makaleleri
Yazarlar

Bahattin Güllü 0000-0002-3629-1124

Hacer Bilgilioğlu 0000-0002-8629-1077

Proje Numarası BAP-2015-077
Erken Görünüm Tarihi 18 Ekim 2023
Yayımlanma Tarihi 27 Ekim 2023
Yayımlandığı Sayı Yıl 2023 Cilt: 5 Sayı: 2

Kaynak Göster

APA Güllü, B., & Bilgilioğlu, H. (2023). Sarıcakaya (Eskişehir) Granitoyidindeki Pegmatitlerin Kökeni ve Endüstriyel Hammadde Potansiyeli. Mühendislik Bilimleri Ve Araştırmaları Dergisi, 5(2), 371-382. https://doi.org/10.46387/bjesr.1347030
AMA Güllü B, Bilgilioğlu H. Sarıcakaya (Eskişehir) Granitoyidindeki Pegmatitlerin Kökeni ve Endüstriyel Hammadde Potansiyeli. Müh.Bil.ve Araş.Dergisi. Ekim 2023;5(2):371-382. doi:10.46387/bjesr.1347030
Chicago Güllü, Bahattin, ve Hacer Bilgilioğlu. “Sarıcakaya (Eskişehir) Granitoyidindeki Pegmatitlerin Kökeni Ve Endüstriyel Hammadde Potansiyeli”. Mühendislik Bilimleri Ve Araştırmaları Dergisi 5, sy. 2 (Ekim 2023): 371-82. https://doi.org/10.46387/bjesr.1347030.
EndNote Güllü B, Bilgilioğlu H (01 Ekim 2023) Sarıcakaya (Eskişehir) Granitoyidindeki Pegmatitlerin Kökeni ve Endüstriyel Hammadde Potansiyeli. Mühendislik Bilimleri ve Araştırmaları Dergisi 5 2 371–382.
IEEE B. Güllü ve H. Bilgilioğlu, “Sarıcakaya (Eskişehir) Granitoyidindeki Pegmatitlerin Kökeni ve Endüstriyel Hammadde Potansiyeli”, Müh.Bil.ve Araş.Dergisi, c. 5, sy. 2, ss. 371–382, 2023, doi: 10.46387/bjesr.1347030.
ISNAD Güllü, Bahattin - Bilgilioğlu, Hacer. “Sarıcakaya (Eskişehir) Granitoyidindeki Pegmatitlerin Kökeni Ve Endüstriyel Hammadde Potansiyeli”. Mühendislik Bilimleri ve Araştırmaları Dergisi 5/2 (Ekim 2023), 371-382. https://doi.org/10.46387/bjesr.1347030.
JAMA Güllü B, Bilgilioğlu H. Sarıcakaya (Eskişehir) Granitoyidindeki Pegmatitlerin Kökeni ve Endüstriyel Hammadde Potansiyeli. Müh.Bil.ve Araş.Dergisi. 2023;5:371–382.
MLA Güllü, Bahattin ve Hacer Bilgilioğlu. “Sarıcakaya (Eskişehir) Granitoyidindeki Pegmatitlerin Kökeni Ve Endüstriyel Hammadde Potansiyeli”. Mühendislik Bilimleri Ve Araştırmaları Dergisi, c. 5, sy. 2, 2023, ss. 371-82, doi:10.46387/bjesr.1347030.
Vancouver Güllü B, Bilgilioğlu H. Sarıcakaya (Eskişehir) Granitoyidindeki Pegmatitlerin Kökeni ve Endüstriyel Hammadde Potansiyeli. Müh.Bil.ve Araş.Dergisi. 2023;5(2):371-82.