Magma interaction processes inferred from Fe-Ti oxide compositions in the Dölek and Sarıçiçek plutons, Eastern Turkey

Orhan KARSLI, (Karadeniz Teknik Üniversitesi, Mühendislik Fakültesi, Jeoloji Mühendisliği Bölümü, Trabzon, Türkiye)
Faruk AYDIN, (Niğde Üniversitesi, Mühendislik Mimarlık Fakültesi, Jeoloji Mühendisliği Bölümü, Niğde, Türkiye)
İbrahim UYSAL, (Karadeniz Teknik Üniversitesi, Mühendislik Fakültesi, Jeoloji Mühendisliği Bölümü, Trabzon, Türkiye)
M. Burhan SADIKLAR (Karadeniz Teknik Üniversitesi, Mühendislik Fakültesi, Jeoloji Mühendisliği Bölümü, Trabzon, Türkiye)
Turkish Journal of Earth Sciences
4 0
Yıl: 2008 Cilt: 17 Sayı: 2 Sayfa Aralığı: 297 - 315 Metin Dili: Türkçe İndeks Tarihi: 29-07-2022

Magma interaction processes inferred from Fe-Ti oxide compositions in the Dölek and Sarıçiçek plutons, Eastern Turkey

Öz:
Doğu Türkiye’de, yüksek-K’lu kalk-alkalin Dölek ve Sarıçiçek plütonlarındaki manyetit-ulvospinel ve ilmenithematit katı ergiyik ürünleri mikroprop analizleri ile incelenmiştir. Oksijen kısmi basıncı ve sıcaklık tahminleri için, plütonlarda anklav ve ana kayaçlardan toplanan yirmi sekiz örneğin bileşimleri kullanılmıştır. İlmenit ve ulvöspinel, ana kayaçlardaki titanomanyetitlerde bazı kristalografik yüzeyler boyunca düzenli bir biçimde ayrılım lamelleri halinde oluşmuşlardır. Ancak, bu oluşum, mafik mikrogranular enklavların titanomanyetitlerinde bulunmamaktadır. Titanomanyetit ve ilmenit sırasıyla, $Mt_{98-70}Usp_{02-30}$ ve $Ilm_{99-65}Hm_{01-35}$ bileşimindedir. Titanomanyetit-ilmenit termometre/oksijen barometresi kullanılarak elde edilen oksijen fugasitesi tahminleri, ana kayaçlarda -15.30 logfO2 ila -20.48 log fO2 arasında, mafik mikrogranular enklavlarda -15.39 log fO2 ila -20.80 log fO2 arasındadır. Sıcaklık tahminleri ise, ana kayaçlarda; 617 ± 6 ila 758±23 °C arasında, mafik mikrogranular enklavlarda ise 622±6 ile 735±24 °C arasındadır. Sıcaklık değerleri, yüksek olasılıkla kristalleşme sırasındaki değerlerini temsil ederler. Granitoyid kayaçlar üzerinde yapılan bu titanomanyetit-ilmenit jeotermometresi, lamel biçimli ilmenit çiftleri üzerinde de denenmiştir ve ortalama 679±18 °C oluşum sıcaklığı belirlenmiştir. Fe-Ti oksitlerin spesifik kristal biçimleri, kimyasal özellikleri ve ana kayaç ve mafik mikrogranular anklavlardan (MME) alınan Fe-Ti oksit çiftlerinden hasaplanan sıcaklık ve oksijen fugasitesi değerlerindeki benzerlikler, bu plütonların kristalizasyonu süresince, dinamik bir magma odasında muhtemelen bir felsik ile bir mafik magmanın çeşitli oranlarda karışmış olabileceğini ve bu iki tezat magma arasında yüksek olasılıkla termal dengenin sağlanmış olabileceğine işaret etmektedir. Hibrit plütonların oluşumlarında, büyük olasılıkla, yükselen sıcak magmanın manto-kabuk sınırına yerleşerek magma odası oluşturması mekanizması etkili olmuştur. Litosferik üst manto (mafik uç üye) ve alt kabuktan (felsik uç üye) türeyen eşyaşlı magmaların karışabilme modelinin gerçekleşebilmesi için sıcaklık kaynağının tanımlanması gerekir. Sıcak astenosferin yükselmesi neticesinde, sıcaklık değişimi meydana gelir ve litosferik manto ergimiş olabilir. Daha sonra, litosferik mantodan türeyen sıcak magma alt kabuğu ergitir ve felsik magma meydana gelir. Alt kabuk ve üst manto kaynaklı magmaların karışımı bu hibrit plütonları oluşturmuştur. Bu olay Doğu Pontidler’de Eosen sürecinde, çarpışma sonrası genişlemeli bir tektonik ortamın varlığını gerektirir.
Anahtar Kelime:

Konular: Jeoloji

Dölek ve Sarıçiçek plütonlarındaki Fe-Ti oksit bileşimlerinde magma karışım izleri, Doğu Türkiye

Öz:
Abstract: Magnetite-ulvöspinel and ilmenite-hematite solid solution intergrowths from the high-K calc-alkaline Dölek and Sarıçiçek plutons, Eastern Turkey, were investigated using microprobe analyses. Compositions of twenty-eight samples from the host rocks and their enclaves in the plutons were used to estimate the oxygen fugacity and temperature. The ilmenite and ulvöspinel component exsolves out along certain preferred crystallographic planes in the titanomagnetite of the host rocks, while they are always absent in those of the mafic microgranular enclaves. The titanomagnetite and ilmenite show variations as $Mt_{98-70}Usp_{02-30}$ and $Ilm_{99-65}Hm_{01-35}$ in composition, respectively. Estimations of oxygen fugacity and temperature using the titanomagnetite-ilmenite thermometry/oxygen barometry range from log fO2 of -15.30 to -20.48 in host rocks, logfO2 of -15.39 to -20.80 in the mafic microgranular enclaves and 617±6 to 758±23 °C in host rocks, 622±6 to 735±24 °C in the mafic microgranular enclaves, possibly indicating crystallisation temperature. Applying magnetite-ilmenite thermometry/oxygen barometry to the granitoid rocks also involves microprobe analyses of ilmenite lamellae in titanomagnetite and this method yielded mean temperatures of 679±18 °C. The specific forms and chemical properties of Fe-Ti oxides, and similarities in crystallization temperature and oxygen fugacity of the host rocks and the mafic microgranular enclaves (MME) obtained from the Fe-Ti oxide pairs imply that thermal equilibrium probably occurred between two contrasted magmas, which mixed in various proportions so that possibly a felsic and a more mafic magma interaction occurred in a convectively dynamic magma chamber during crystallization of the plutons. Probably, underplating may be responsible for genesis of the hybrid plutons. Thus, for mixing of coeval magmas derived from a lithospheric upper mantle (mafic end-member) and lower crust (felsic end-member), a thermal anomaly should be supplied. Upwelling of hot asthenospheric material results in thermal perturbation and melting of lithospheric mantle. Intrusion of hot lithospheric mantle-derived mafic magma then induced lower crustal melting, producing felsic melt. Mixing of the lower crust-derived melt and lithospheric mantle-derived magma formed the hybrid plutons. This process requires a post-collisional extensional tectonic setting during the Eocene in the Eastern Pontides.
Anahtar Kelime:

Konular: Jeoloji
Belge Türü: Makale Makale Türü: Araştırma Makalesi Erişim Türü: Erişime Açık
  • AKIN, H. 1979. Geologie, magmatismus und Lagerstattenbildung im ostpontischen Gebirge/Türkei aus der Sicht der Plattentektonik. Geolgische Rundschau 68, 253–283.
  • ANDERSEN, D.J., BISHOP, F.C. & LINDSLEY, D.H. 1991. Internally consistent solution models for Fe-Mg-Mn-Ti oxides: Fe-Mg-Ti oxides and olivine. American Mineralogist 76, 427–444.
  • AYDIN, F., KARSLI, O. & SADIKLAR, M.B. 2003. Mineralogy and chemistry of biotites from eastern Pontide granitoid rocks, NE Turkey: Some petrological implications for granitoid magmas. Chemie der Erde-Geochemistry 63, 163–182.
  • BARBARIN, B. & DIDIER, J. 1992. Genesis and evolution of mafic microgranular enclaves through various types of interaction between coexisting felsic and mafic magmas. Transactions of the Royal Society of Edinburgh, Earth Science 83, 145–153.
  • BLUNDY, J.D. & HOLLAND, T.J.B. 1990. Calcic amphibole equilibria and a new amphibole-plagioclase geothermometer. Contributions to Mineralogy and Petrology 104, 208–224.
  • BOZTUĞ, D., JONCKHEERE, R., WAGNER, G.A. & YEĞiNGİL, Z. 2004. Slow Senonian and fast Paleocene–Early Eocene uplift of the granitoids in the central eastern Pontides, Turkey: Apatite fission-track results. Tectonophysics 382, 213–228.
  • BOZTUĞ, D., ERÇİN, A.I., KURUÇELİK, M.K., GÖÇ, D., KÖMÜR, I. & İSKENDEROĞLU, A. 2006. Main geochemical characteristics of the composite Kaçkar batholith derived from the subduction through collision to extentional stages of Neo-Tethyan convergence system in the Eastern Pontides, Turkey. Journal of Asian Earth Sciences 27, 286–302.
  • BOZTUĞ, D. & HARLAVAN, Y. 2007. K-Ar ages of granitoids unravel the stages of Neo-tethyan convergence in the eastern Pontides and central Anatolia, Turkey. International Journal of Earth Sciences, doi:10.1007/s00531-007-0176-0.
  • BOZTUĞ, D., JONCKHEERE, R., WAGNER, G.A., ERÇİN, A.I. & YEĞİNGİL, Z. 2007. Titanite and zircon fission-track dating resolves successive igneous episodes in the formation of the composite Kaçkar batholith in the Turkish eastern Pontides. International Journal of Earth Science 96, 875–886.
  • DEVINE, J.D., RUTHERFORD, M.J., NORTON, G.E. & YOUNG, S.R. 2003. Magma storage region processes inferred from geochemistry of Fe-Ti oxides in andesitic magma, Soufriere Hills Volcano, Montserrat, W.I. Journal of Petrology 44, 1375–1400.
  • DIDIER, J. & BARBARIN, B. 1991. Review of the main hypotheses proposed for the genesis and evoluation of mafic microgranular enclaves. In: DIDIER, J. & BARBARIN, B. (eds), Enclaves and Granite Petrology, Developments in Petrology. Amsterdam 13, 367–373.
  • DOKUZ, A., TANYOLU, E. & GENÇ, S. 2006. A mantle- and a lower crustderived bimodal suite in the Yusufeli (Artvin) area, NE Turkey: trace element and REE evidence for subduction-related rift origin of Early Jurassic Demirkent intrusive complex. International Jounal of Earth Sciences 95, 370–394.
  • ELBURG, M.A. 1996. Evidence of isotopic equilibration between microgranitoid enclaves and host granodiorite, Warburton Granodiorite, Lachlan Fold Belt, Australia. Lithos 38, 1–22.
  • FERNANDEZ, A.N. & BARBARIN, B. 1991. Relative rheology of coexisting mafic and felsic magmas: Nature of resulting interaction processes. Shape and mineral fabrics of mafic microgranular enclaves. In: DIDIER, J. & BARBARIN, B. (eds), Enclaves and Granite Petrology, Developments in Petrology. Amsterdam 13, 263–275.
  • FROST, B.R. & LINDSLEY, D.H. 1991. The occurrence of iron-titanium oxides in igneous rocks. In: LINDSLEY, D.H. (ed), Oxide Minerals: Petrologic and Magnetic Significance. Reviews in Mineralogy, Mineralogical Society of America, Washington 25, 433–468.
  • FROST, B.R., LINDSLEY, D.H. & ANDERSEN, D.J. 1988. Fe-Ti oxide-silicate equilibria: Assemblages with fayalitic olivine. American Mineralogist 73, 727–740.
  • FROST, B.R. & MAHOOD, G.A. 1987. Field, chemical and physical constraints on mafic-felsic interaction in the Lamarck granodiorite, Sierra Nevada, California. Geological Society of America Bulletin 99, 272–291.
  • GEDİK, A., ERCAN, T., KORKMAZ, S. & KARATAŞ, S. 1992. Rize-Fındıklı-Çamlihemşin arasında (Doğu Karadeniz) yer alan magmatik kayaçların petrolojisi ve Doğu Pontidlerdeki bölgesel yayılımları [Petrology of the magmatic rocks around Rize-Fmdıklı-Çamlıhemşin (Eastern Black Sea) and their distribution at the Eastern Pontides]. Geological Bulletin of Turkey 35, 15–38 [in Turkish with English abstract].
  • GHIORSO, M.S. & SACK, R.O. 1991. Fe-Ti oxide geothermometry: thermodynamic formulation and the estimation of intensive variables in silicic magmas. Contributions to Mineralogy and Petrology 108, 485–510.
  • HAGGERTY, S.E. 1991. Oxide textures-a mini atlas. In: LINDSLEY, D.H. (ed), Oxide Minerals: Petrologic and Magnetic Significance. Reviews in Mineralogy, Mineralogical Society of America, Washington 25, 129–219.
  • HAMMOND, P.A. & TAYLOR, L.A. 1982. The ilmenite/titano-magnetite assemblage: Kinetics of re-equilibration. Earth and Planetary Science Letters 61, 143–150.
  • HARLOV, D.H. 1992. Comparative oxygen barometry in granulites, Bamble sector, SE Norway. Journal of Geology 100, 447–464.
  • HARLOV, D.E. 2000. Titaniferous magnetite-ilmenite thermometry and titaniferous magnetite-ilmenite-orthopyroxene-quartz oxygen barometry in granulite facies gneisses, Bamble Sector, SE Noway: Implications for the role of high-grade CO2-rich fluids during granulite genesis. Contributions to Mineralogy and Petrology 1139, 180–197.
  • HUEBNER, J.S. & SATO, M. 1970. The oxygen fugacity-temperature relationships of manganese oxide and nickel oxide buffers. American Mineralogist 55, 934–952.
  • HIBBARD, M.J. 1991. Textural anatomy of twelve magma-mixed granitoid systems. In: DIDIER, J. & BARBARIN, B. (eds), Enclaves and Granite Petrology, Developments in Petrology. Amsterdam 13, 431–444.
  • HOLDEN, P., HALLIDAY, A.N., STEPHENS, W.E. & HENNEY, P.J. 1991. Chemical and isotopic evidence for major mass transfer between mafic enclaves and felsic magma. Chemical Geology 92, 135–152.
  • KARSLI, O., AYDIN, F. & SADIKLAR, M.B. 2002. Geothermobarometric investigation of the Zigana Granitoid, eastern Pontides, Turkey. International Geology Review 44, 277–286.
  • KARSLI, O. 2002. Granitoyid Kayaçlarda Magma Etkileşimleri için Petrografik, Mineralojik ve Kimyasal Bulgular: Dölek ve Sariçiçek Plutonları (Gümüşhane, KD-Türkiye) [Petrographic, Mineralogic and Chemical Evidence for Magma Interaction in Granitoid Rocks: Dölek and Sarıçiçek Plutons (Gümüşhane, NE Turkey)]. PhD Thesis, Karadeniz Technical University, Trabzon, Turkey [in Turkish with English abstract, unpublished].
  • KARSLI, O., AYDIN, F. & SADIKLAR, M.B. 2004a. Magma interaction recorded in plagioclase zoning in granitoid systems, Zigana Granitoid, Eastern Pontides, Turkey. Turkish Journal of Earth Sciences 13, 287–305.
  • KARSLI, O., AYDIN, F. & SADIKLAR, M.B. 2004b. The morphology and chemistry of K-feldspar megacrysts from İkizdere Pluton: evidence for acid and basic magma interactions in granitoid rocks, NE Turkey. Chemie der Erde-Geochemistry 64, 155–170.
  • KARSLI, O., CHEN, B., AYDIN, F. & ŞEN, C. 2007. Geochemical and Sr-Nd- Pb isotopic compositions of the Eocene Dölek and Sarıçiçek Plutons, Eastern Turkey: Implications for magma interaction in the genesis of high-K calc-alkaline granitoids in a post-collision extensional setting. Lithos 98, 67–96.
  • KUMAR, S., RINO, V. & PAL, A.B. 2004. Field evidence of magma mixing from microgranular enclaves hosted in Palaeoproterozoic Malanjkhand granitoids, Central India. Gondwana Research 7, 539–548.
  • LINDSLEY, D.H. 1981. Some experiment pertaining to the magnetiteulvöspinel miscibility gap. American Mineralogist 66, 759–762.
  • LINDSLEY, D.H., FROST, B.R., ANDERSEN, D.J. & DAVIDSON, P.M. 1990. Fe- Ti oxide-silicate equilibria: assemblages with orthopyroxene. In: SPENCER, R.J. & CHOU, I.M. (eds), Fluid-mineral Interactions: A Tribute to EUGSTER H.P. The Geochemical Society Publication 2, 103–119.
  • MOORE, W.J., MCKEE, E.H. & AKINCI, Ö. 1980. Chemistry and chronology of plutonic rocks in the Pontide Mountains, Northern Turkey. Symposium of European Copper Deposit, Belgrade, 209–216.
  • NAKAMURA, M. 1995. Continious mixing of crystal mush and replenished magma in the ongoing Unzen eruption. Geology 23, 807–810.
  • OKAY, A.I. & ŞAHİNTÜRK, Ö. 1997. Geology of the Eastern Pontides. In: ROBINSON, A.G. (ed), Regional and Petroleum Geology of the Black Sea and Surrounding Region. American Association Petroleum Geologist Memoir 68, 291–310.
  • OKAY, A.‹., ŞAHİNTÜRK, Ö. & YAKAR, H. 1997. Stratigraphy and tectonics of the Pulur (Bayburt) region in the Eastern Pontides. Mineral Research and Exploration Institute (MTA) of Turkey Bulletin 119, 1–24.
  • PERUGINI, D. & POLI, G. 2000. Chaotic dynamics and fractals in magmatic interaction processes: A different approach to the interpretation of mafic microgranular enclaves. Earth and Planetary Science Letters 175, 93–103.
  • PERUGINI, D., POLI, G., CHRISTOFIDES, G. & ELEFTHERIADIS, G. 2003. Magma mixing in the Sithonia Plutonic Complex, Greece: evidence from mafic microgranular enclaves. Mineralogy and Petrology 78, 173–200.
  • PERUGINI, D., VENTURA, G., PETRELLI, M. & POLI, G. 2004. Kinematic significance of morphological structures generated by mixing of magmas: a case study from Salina Island (southern Italy). Earth and Planetary Science Letters 222, 1051–1066. POLI, G.E. & TOMMASINI, S. 1991. Model for the origin and significance of microgranular enclaves in calc-alkaline granitoids. Journal Petrology 32, 657–666.
  • POLI, G.E. & TOMMASINI, S. 1999. Geochemical modelling of acid-basic magma interaction in the Sardinia-Corsica Batholith: The case study of Sarrabus, Southeastern Sardinia, Italy. Lithos 46, 553–571.
  • POUCHOU, J.L. & PICHOIR, F. 1985. ‘PAP’ (ø.ρ.Z) correction procedure for improved quantitative microanalysis. In: ARMSTRONG, J.T. (ed), Microbeam Analysis. San Francisco Press 104–106.
  • PRICE, G.D. 1981. Subsolidus phase relations in the titanomagnetite solid solution series. American Mineralogist 66, 751–758.
  • ROBINSON, A.G., BANKS, C.J., RUTHERFORD, M.M. & HIRST, J.P.P. 1995. Stratigraphic and structural development of the Eastern Pontides, Turkey. Journal of the Geological Society, London 152, 861–872.
  • SADIKLAR, M.B. & HANEDAN, A. 1997. Entmischte Magnetite in Obsidian (Ikizdere/NE-Turkei) und deren Genetische Bedeutung. Beihefte zum European Journal of Mineralogy 9, p. 301.
  • ŞAHİN, S.Y., GÜNGÖR, Y. & BOZTUĞ, D. 2004. Comparative petrogenetic investigation of composite Kaçkar Batholith granitoids in Eastern Pontide magmatic arc-Northern Turkey. Earth Planets and Space 56, 429–446.
  • ŞEN, C., ARSLAN, M. & VAN, A. 1998. Geochemical and petrological characteristics of the Eastern Pontide Eocene (?) alkaline volcanic province, NE Turkey. Turkish Journal of Earth Sciences 7, 231–239.
  • ŞENGÖR, A.M.C. & YILMAZ, Y. 1981. Tethyan evolution of Turkey: a plate tectonic approach. Tectonophysics 75, 181–241.
  • ŞENGÖR, A.M.C., ÖZEREN, S., GENÇ, T. & ZOR, E. 2003. East Anatolian high plateau as a mantle-supported, north-south shortened domal structure. Geophysical Research Letters 30 (24), 8044, doi:10.1029/2003GL018192.
  • SPENCER, K.J. & LINDSLEY, D.H. 1981. A solution model for coexisting iron-titanium oxides. American Mineralogist 66, 1189–1201.
  • TANER, M.F. 1977. Etude geologique et petrographique de la region de Güneyce-İkizdere, situee au sud de Rize (Pontides orientalas, Turquie). PhD Thesis, Université de Geneve, Switzerland [unpublished].
  • TOKEL, S. 1977. Eocene calc-alkaline andesites and geotectonism in the Eastern Black Sea region. Geological Bulletin of Turkey 20, 49–54 [in Turkish with English abstract].
  • TOPUZ, G., ALTHERR, R., SCHWARZ, W.H., SIEBEL, W., SATIR, M. & DOKUZ, A. 2005. Post-collisional plutonism with adakite-like signatures: the Eocene Saraycık granodiorite (Eastern Pontides, Turkey). Contributions to Mineralogy and Petrology 150, 441–455.
  • TOPUZ, G. & OKAY, A.İ. 2006. Comment on Petrography and petrology of the calc-alkaline Sarıhan Granitoid (NE-Turkey): An example of magma mingling and mixing. Turkish Journal of Earth Sciences 15, 373–377.
  • VENEZKY, D.Y. & RUTHERFORD, M.J. 1999. Petrology and Fe-Ti oxide reequilibration of the 1991 Mount Unzen mixed magma. Journal of Volcanology and Geothermal Research 89, 213–230.
  • VERNON, R.H. 1984. Microgranitoid enclaves in granites-globules of hybrid magma quenched in a plotonic environment. Nature 309, 438–439.
  • VERNON, R.H. 1990. Crystallization and hybridisation in microgranitoid enclave magmas: microstructural evidence. Journal of Geophysical Research 95, 17849–17859.
  • WAIGHT, T.E., MAAS, R. & NICHOLLS, I.A. 2000. Fingerprinting feldspar phenocrysts using crystal isotopic composition stratigraphy: Implications for crystal and magma mingling in S-type granites. Contributions to Mineralogy and Petrology 139, 227–239.
  • WIEBE, R.A. 1980. Commingling of contrasted magmas in the plutonic environment: Examples from The Nain Anorthositic Complex. Journal of Geology 88, 197–209.
  • YILMAZ, Y. 1972. Petrology and Structure of the Gümüşhane Granite and Surrounding Rocks, North-eastern Anatolia. PhD Thesis, University of London, England [unpublished].
  • YILMAZ, S. & BOZTUĞ, D. 1996. Space and time relations of three plutonic phase in the eastern Pontides, Turkey. International Geology Review 38, 935–956.
  • YILMAZ, Y., TÜYSÜZ, O., YİĞİTBAŞ, E., GENÇ, Ş.C. & ŞENGÖR, A.M.C. 1997. Geology and tectonic evolution of the Pontides. In: ROBINSON, A.G. (ed), Regional and Petroleum Geology of the Black Sea and Surrounding Region. American Association Petroleum Geologist Memoir 68, 183–226.
  • YILMAZ, C. & KANDEMİR, R. 2006. Sedimentary records of the extensional tectonic regime with temporal cessation: Gümüşhane Mesozoic Basin (NE-Turkey). Geologica Carpathica 57, 3–13.
APA KARSLI O, Aydın F, UYSAL İ, SADIKLAR M (2008). Magma interaction processes inferred from Fe-Ti oxide compositions in the Dölek and Sarıçiçek plutons, Eastern Turkey. , 297 - 315.
Chicago KARSLI Orhan,Aydın Faruk,UYSAL İBRAHİM,SADIKLAR M. Burhan Magma interaction processes inferred from Fe-Ti oxide compositions in the Dölek and Sarıçiçek plutons, Eastern Turkey. (2008): 297 - 315.
MLA KARSLI Orhan,Aydın Faruk,UYSAL İBRAHİM,SADIKLAR M. Burhan Magma interaction processes inferred from Fe-Ti oxide compositions in the Dölek and Sarıçiçek plutons, Eastern Turkey. , 2008, ss.297 - 315.
AMA KARSLI O,Aydın F,UYSAL İ,SADIKLAR M Magma interaction processes inferred from Fe-Ti oxide compositions in the Dölek and Sarıçiçek plutons, Eastern Turkey. . 2008; 297 - 315.
Vancouver KARSLI O,Aydın F,UYSAL İ,SADIKLAR M Magma interaction processes inferred from Fe-Ti oxide compositions in the Dölek and Sarıçiçek plutons, Eastern Turkey. . 2008; 297 - 315.
IEEE KARSLI O,Aydın F,UYSAL İ,SADIKLAR M "Magma interaction processes inferred from Fe-Ti oxide compositions in the Dölek and Sarıçiçek plutons, Eastern Turkey." , ss.297 - 315, 2008.
ISNAD KARSLI, Orhan vd. "Magma interaction processes inferred from Fe-Ti oxide compositions in the Dölek and Sarıçiçek plutons, Eastern Turkey". (2008), 297-315.
APA KARSLI O, Aydın F, UYSAL İ, SADIKLAR M (2008). Magma interaction processes inferred from Fe-Ti oxide compositions in the Dölek and Sarıçiçek plutons, Eastern Turkey. Turkish Journal of Earth Sciences, 17(2), 297 - 315.
Chicago KARSLI Orhan,Aydın Faruk,UYSAL İBRAHİM,SADIKLAR M. Burhan Magma interaction processes inferred from Fe-Ti oxide compositions in the Dölek and Sarıçiçek plutons, Eastern Turkey. Turkish Journal of Earth Sciences 17, no.2 (2008): 297 - 315.
MLA KARSLI Orhan,Aydın Faruk,UYSAL İBRAHİM,SADIKLAR M. Burhan Magma interaction processes inferred from Fe-Ti oxide compositions in the Dölek and Sarıçiçek plutons, Eastern Turkey. Turkish Journal of Earth Sciences, vol.17, no.2, 2008, ss.297 - 315.
AMA KARSLI O,Aydın F,UYSAL İ,SADIKLAR M Magma interaction processes inferred from Fe-Ti oxide compositions in the Dölek and Sarıçiçek plutons, Eastern Turkey. Turkish Journal of Earth Sciences. 2008; 17(2): 297 - 315.
Vancouver KARSLI O,Aydın F,UYSAL İ,SADIKLAR M Magma interaction processes inferred from Fe-Ti oxide compositions in the Dölek and Sarıçiçek plutons, Eastern Turkey. Turkish Journal of Earth Sciences. 2008; 17(2): 297 - 315.
IEEE KARSLI O,Aydın F,UYSAL İ,SADIKLAR M "Magma interaction processes inferred from Fe-Ti oxide compositions in the Dölek and Sarıçiçek plutons, Eastern Turkey." Turkish Journal of Earth Sciences, 17, ss.297 - 315, 2008.
ISNAD KARSLI, Orhan vd. "Magma interaction processes inferred from Fe-Ti oxide compositions in the Dölek and Sarıçiçek plutons, Eastern Turkey". Turkish Journal of Earth Sciences 17/2 (2008), 297-315.
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22-04-2024 13:3

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