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Geochemistry and Petrology of Tutak (Ağrı) Volcanic Rocks: Partial Melting of Amphibole Bearing Garnet Peridotite

Year 2018, Volume: 33 Issue: 3, 41 - 56, 30.09.2018
https://doi.org/10.21605/cukurovaummfd.500540

Abstract

The Pliocene aged Tutak volcanic rocks located in the northeast of Turkey is one of the most important basaltic plateaus related to the collision in the East Anatolia. Volcanic products have basaltic compositions and they plot on alkaline-sub-alkaline division line. All of the basaltic lavas composed of olivine, pyroxene, plagioclase and opaque mineral phenocrystals and microlites, displaying intersertal, subophitic and flow textures. Fractional crystallisation and EC-RAFC (Energy-constrained assimilation, fractional crystallisation and magma recharge) models indicate that fractional crystallisation and crustal contamination play an important role in the evolution of the Tutak volcanic rocks. Lower 144Nd/143Nd and higher 87Sr/86Sr isotopic ratios and enrichment of large ion lithophile elements (LILE) and light rare earth elements (LREE) relative to high strength field elements (HFSE) of the least evolved basaltic samples indicate that the mantle source region might be enriched by melts that were derived from subducted sediments. Partial melting models generated by using rare earth element systematics calculations show that basaltic melts might have been produced by melting of a metasomatised mantle source containing both amphibole and garnet with a partial melting degree between 0.2 and 2%.  

References

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Tutak (Ağrı) Volkanitlerinin Jeokimyası ve Petrolojisi: Amfibolce Zengin Granat Peridotitin Kısmi Ergimesi

Year 2018, Volume: 33 Issue: 3, 41 - 56, 30.09.2018
https://doi.org/10.21605/cukurovaummfd.500540

Abstract

Türkiye’nin kuzeydoğusunda yer alan Pliyosen yaşlı Tutak volkanitleri, Doğu Anadolu Bölgesi’nde çarpışmayla ilişkili en önemli bazaltik platolardan biridir. Volkanik ürünler bazaltik bileşime sahiptirler ve alkali-subalkali ayrım çizgisi üzerine iz düşerler. Bazaltik kayaçların tamamı olivin, piroksen, plajiyoklaz ve opak mineral fenokristalleri ve mikrolitlerinden oluşur ve intersertal, subofitik ve akma dokuları sergilerler. Fraksiyonel kristallenme ve EC-AFC (enerjiye bağımlı fraksiyonel kristallenme, ile birleşik asimilasyon) modelleri Tutak volkanitlerinin evriminde fraksiyonel kristallenme ve kıtasal kirlenmenin önemli rol oynadıklarına işaret eder. En az evrimleşmiş (yüksek MgO içerikli lavlar) bazaltik örneklerinin düşük 143Nd/144Nd ve yüksek 87Sr/86Sr izotopik oranları ile büyük iyon yarıçaplı litofil (BİYÇL) ve hafif nadir toprak elementlerinin (HNTE), yüksek alan şiddetli elementlerine (YAŞE) göre belirgin zenginleşmesi, manto kaynak alanında yitim bileşeninin varlığına ve baskın olarak sediment ergimeleri ile zenginleştiğine işaret eder. Nadir torak element sistematiğinin kullanılması ile üretilen kısmi ergime modelleri, bazaltik ergiyiklerin kısmi ergime derecesi %0,7 ile %2 arasında değişen ve amfibol ile granat içeren metasomatize olmuş manto kaynağının ergimesi ile üretilebileceğini göstermiştir. 

References

  • 1. Pearce, J.A., Bender, J.F., De long, S.E., Kidd, W.S.F., Low, P.J., Güner, Y., Şaroğlu, F., Yılmaz, Y., Moorbath, S., Mitchell, G.J., 1990. Genesis of Collision Volcanism in Eastern Anatolia, Turkey. Journal of Volcanology and Geothermal Research, 44,189-229.
  • 2. Keskin, M., Pearce, J.A., Mitchell, J.G., 1998. Volcano-stratigraphy and Geochemistry of Collision-related Volcanism on the Erzurum- Kars Plateau, North Eastern Turkey, Joural of Volcanology and Geothermal Research, 85, 355-404.
  • 3. Keskin, M., 2003. Magma Generation by Slab Steepening and Breakoff Beneath a Subduction-accretion Complex: An Alternative Model for Collision-related Volcanism in Eastern Anatolia, Turkey. Geophysical Research Letter, 30, 8046-8050.
  • 4. Allen, M.B., Kheirkhah, M., Neill, I., Emami, M.H., McLeod, C.L., 2013. Generation of Arc and Within-plate Chemical Signatures in Collision Zone Magmatism: Quaternary Lavas from Kurdistan Province, Iran. Journal of Petrology, 54, 887–911.
  • 5. Neill, I., Meliksetian, Kh., Allen, M.B., Navarsardyan, G., Karapetyan, S., 2013. Pliocene–Quaternary Volcanic Rocks of NW Armenia: Magmatism and Lithospheric Dynamics Within an Active Orogenic Plateau. Lithos, 180–181, 200–215.
  • 6. Neill, I., Meliksetian, Kh., Allen, M.B., Navarsardyan, G., Kuiper, K., 2015. Petrogenesis of Mafic Collision Zone Magmatism: The Armenian Sector of the Turkish–Iranian Plateau. Chemical Geology, 403, 24-41.
  • 7. Oyan, V., Keskin, M., Lebedev, V.A., Chugaev, A.V., Sharkov, E.V., 2016. Magmatic Evolution of the Early Pliocene Etrüsk Stratovolcano, Eastern Anatolia Collision Zone, Turkey. Lithos, 256-257, 88-108.
  • 8. Lebedev, V.A., Sharkov, E.V., Ünal, E., Keskin, M., 2016. Late Pleistocene Tendürek Volcano (Eastern Anatolia, Turkey): II. Geochemistry and Petrogenesis of the Rocks. Petrology, 24, 234-270.
  • 9. Şengör, A.M.C., Özeren, S., Zor, E., Genç, T., 2003. East Anatolian High Plateau as a Mantlesupported, N-S Shortened Domal Structure. Geophysical Research Letter, 30, 8043-8045.
  • 10. Şengör, A.M.C., Özeren, S., Keskin, M., Sakınç, M., Özbakır, A.D., ve Kayan, I., 2008. Eastern Turkish High-plateau as a Small Turkish Type Orogen: Implications for Postcollisional Crust-forming Processes in Turkic Type Orogens, Earth sciences Rewievs, 90, 1-48.
  • 11. Yılmaz, Y., Şaroğlu, F., Güner, Y., 1987. Initation of the Neomagmatism in East Anatolia. Tectonophysics, 137,177-199.
  • 12. Okay, A.I., Zatin, M., Cavazza, V., 2010. Apatite Fission-track Data for the Miocene Arabia-Eurasia Collision. Geology, 38, 35-38.
  • 13. Karaoğlan, F., Parlak, O., Thöni, M., Klötzli, U., Koller, F., 2016. The Temporal Evolution of the Active Margin Along the Southeast Anatolian Orogenic Belt (SE Turkey): Evidence from U–Pb, Ar-Ar and Fission Track Chronology. Gondwana Research, 33, 190-208.
  • 14. Oyan, V., 2018. Ar-Ar Dating and Petrogenesis of the Early Miocene Taşkapı-Mecitli (Erciş- Van) Granitoid, Eastern Anatolia Collisional Zone, Turkey. Journal of Asian Earth Sciences, 158, 210-226.
  • 15. Lebedev, V, A., Sharkov, E.V., Keskin, M., Oyan, V., 2010. Geochronology of Late Cenezoic Volcanism in the Area of Lake Van, Turkey: An Example of Developmental Dynamics for Magmatic Processes. Doklady Earth Science, 433, 1031-1037.
  • 16. Koçyiğit, A., Yılmaz, A., Adamia, S., Kuloshvili, S., 2001. Neotectonics of East Anatolian Plateau (Turkey) and Lesser Caucasus: Implication for Transition from Thrusting to Strike-slip Faulting. Geodinamica Acta, 14, 177-195.
  • 17. Innocenti, F., Mazzuoli, R., Pasquaré, G., Radicati di Brozolo, F., Villari, L., 1982. Tertiary and Quaternary Volcanism of the Erzurum-Kars area (Eastern Turkey): Geochronological data and Geodynamic Evolution. Joural of Volcanology and Geothermal Research, 13, 223-240.
  • 18. Yılmaz, Y., Güner, Y., Şaroğlu, F., 1998. Geology of the Quaternary Volcanic Centres of the East Anatolia. Journal of Volcanology and Geothermal Research, 137, 177-199.
  • 19. Keskin, M., 2007. Eastern Anatolia: A Hot Spot in a Collision Zone Without a Mantle Plume. GSA Special Paper, 430, 695-722.
  • 20. Özdemir, Y., Güleç, N., 2014. Geological and Geochemical Evoluation of Quaternary Süphan Stratovolcano, Eastern Anatolia, Turkey: Evidence for the Lithosphere-asthenosphere Interaction in Post Collisional Volcanism, Journal of Petrology, 55, 37-62.
  • 21. Oyan, V., Keskin, M., Lebedev, V.A., Chugaev, A.V., Sharkov, E.V., Ünal, E., 2017. Petrology and Geochemistry of the Quaternary Mafic Volcanism in the Northeast of Lake Van, Eastern Anatolian Collision Zone, Turkey. Journal of Petrology, 58, 1701-1728.
  • 22. Köksal, S., Göncüoğlu, M.C., 2008. Sr and Nd Isotopic Characteristics of Some S-I and Atype Granitoids from Central Anatolia. Turkish Journal of Earth Sciences, 17, 111-127.
  • 23. Oyan, V., Özdemir, Y., Jourdan, F., 2015. Petrologic Evolution of Karayazı Basaltic Plateau: Mixture of Melts-derived from Both Spinel and Garnet lherzolite. EGU 2016, 18, 1005, Viyana, Avusturya.
  • 24. Yılmaz, A., Terlemez, İ., Uysal, Ş., 1986. Erzurum’un Güneydoğusunda Yer Alan Hınıs, Tekman ve Karayazı Arasının Jeolojisi ve Volkanik Kayaçların Petrolojisi. Maden Tetkik ve Arama Genel Müdürlüğü Derleme Raporu. Rapor No: 8089, 37.
  • 25. Soytürk, N., 1973. Murat Baseni Jeolojisi ve Hidrokarbon İmkanları Raporu. TPAO Arama Grup Başkanlığı Jeoloji Müdürlüğü Raporu. Rapor No: 791, 22.
  • 26. Oyan, V., 2011. Etrüsk Volkanı ve Çevresinin (Van Gölü Kuzeyi) Volkano Stratigrafisi, Petrolojisi ve Magmatik Evrimi (Doktora tezi, basılmamış). Van YYÜ, Fen Bilimleri Enstitüsü, Van.
  • 27. Le Bas, M.J., Le Maitre, R.W., Streckeisen, A., Zanettin, B., 1986. A Chemical Classification of Volcanic Rocks Based on the Total Alkali– silica Diagram. Journal of Petrology, 27, 745–750.
  • 28. Middlemost, E.A.K., 1975. The Basalt Clan. Earth Science Reviews, 11, 337-364.
  • 29. Peccerillo, A., Taylor, S.R., 1976. Geochemistry of Eocene Calc-alkaline Volcanic Rocks from the Kastamonu Area. Northern Turkey. Contributions to Mineralogy and Petrology, 58, 63–81.
  • 30. Irvine, N., Baragar, W.R.A., 1971. A Guide to Chemical Classification of the Common Volcanic Rocks. Canadian Journal of Earth Science, 8, 523–548.
  • 31. Kuno, H., 1968. Lateral Variation of Basalt Magma Types Across Continental Margins and Island Arcs. Bulletin of Volcanology, 29, 195-222.
  • 32. Sun, S.S., McDonough, W.F., 1989. Chemical and Isotopic Systematics of Oceanic Basalts: Implications for Mantle Composition and Processes. (Magmatism in Ocean Basins, editor Saunders, A.D., Norry, M.J.) Magmatism in Ocean Basins. Geological Society of London Special Publication, 42, 313–345.
  • 33. Keskin, M., Pearce, J.A., Kempton, P.D., Greenwood, P., 2006. Magma–crust Interactions and Mama Plumbing in a Postcollisional Setting: Geochemical Evidence from the Erzurum-Kars Volcanic Plateau, Eastern Turkey. Geological Society of America Special Paper, 409, 475-505.
  • 34. Bohrson, W. A., Spera, F. J., 2001. Energyconstrained Open-system Magmatic Processes II: Application of Energy-constrained Assimilation–fractional Crystallization (ECAFC) Model to Magmatic Systems. Journal of Petrology, 42, 1019–1041.
  • 35. Spera, F.J., Bohrson, W.A., 2001. Energyconstrained Open-system Magmatic Processes I: General Model and Energy-constrained Assimilation and Fractional Crystallization (EC-AFC) Formulation. Journal of Petrology, 42, 999–1018.
  • 36. Taylor, S.R., McLennan, S.M., 1985. The Continental Crust: its Composition and Evolution, Geoscience Texts. Blackwell Scientific Publications, London.
  • 37. Hofmann, A.W., 1997. Mantle Geochemistry: the Message from Oceanic Volcanism. Nature, 385, 219–229.
  • 38. Hawkesworth, C.J., Gallagher, K., Hergt, J. M., McDermott, F., 1993. Mantle and Slab Contributions in Arc Magmas. Annual Review of Earth and Planetary Sciences, 21, 175–204.
  • 39. Hawkesworth, C.J., Turner, S.P., McDermott, F., Peate, D.W., Van Calsteren, P., 1997. U–Th Isotopes in Arc Magmas: Implications for Element Transfer from the Subducted Crust. Science, 276, 551–555.
  • 40. Turner, S., Bourdon, B., Gill, J., 2003. Insight into Magma Genesis at Convergent Margins from U-series Isotopes. In: Bourdon, B., Henderson, G.M., Lundstrom, C.C., Turner, S.P. (eds) Uranium-Series Geochemistry. Reviews in Mineralogy and Geochemistry, Mineralogical Society of America, 52, 255–310.
  • 41. Wang, K.L., Chung, S., O’Reilly, S.Y., Sun, S., Shinjo, R., Chen, C., 2004. Geochemical Constraints for the Genesis of Post-collisional Magmatism and the Geodynamic Evolution of the Northern Taiwan Region. Journal of Petrology, 45, 975-1011.
  • 42. Hasti, A.R., Mitchell, S.F., Treloar, P.J., Kerr, A.C., Neill, I., Barfod, D.N., 2013. Geochemical Components in a Cretaceous Island arc: The Th/La–(Ce/Ce*)Nd Diagram and Implications for Subduction Initiation in the Inter-American Region. Lithos, 162-163, 57-69.
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There are 53 citations in total.

Details

Primary Language Turkish
Subjects Architecture, Engineering
Journal Section Articles
Authors

Vural Oyan

Publication Date September 30, 2018
Published in Issue Year 2018 Volume: 33 Issue: 3

Cite

APA Oyan, V. (2018). Tutak (Ağrı) Volkanitlerinin Jeokimyası ve Petrolojisi: Amfibolce Zengin Granat Peridotitin Kısmi Ergimesi. Çukurova Üniversitesi Mühendislik-Mimarlık Fakültesi Dergisi, 33(3), 41-56. https://doi.org/10.21605/cukurovaummfd.500540
AMA Oyan V. Tutak (Ağrı) Volkanitlerinin Jeokimyası ve Petrolojisi: Amfibolce Zengin Granat Peridotitin Kısmi Ergimesi. cukurovaummfd. September 2018;33(3):41-56. doi:10.21605/cukurovaummfd.500540
Chicago Oyan, Vural. “Tutak (Ağrı) Volkanitlerinin Jeokimyası Ve Petrolojisi: Amfibolce Zengin Granat Peridotitin Kısmi Ergimesi”. Çukurova Üniversitesi Mühendislik-Mimarlık Fakültesi Dergisi 33, no. 3 (September 2018): 41-56. https://doi.org/10.21605/cukurovaummfd.500540.
EndNote Oyan V (September 1, 2018) Tutak (Ağrı) Volkanitlerinin Jeokimyası ve Petrolojisi: Amfibolce Zengin Granat Peridotitin Kısmi Ergimesi. Çukurova Üniversitesi Mühendislik-Mimarlık Fakültesi Dergisi 33 3 41–56.
IEEE V. Oyan, “Tutak (Ağrı) Volkanitlerinin Jeokimyası ve Petrolojisi: Amfibolce Zengin Granat Peridotitin Kısmi Ergimesi”, cukurovaummfd, vol. 33, no. 3, pp. 41–56, 2018, doi: 10.21605/cukurovaummfd.500540.
ISNAD Oyan, Vural. “Tutak (Ağrı) Volkanitlerinin Jeokimyası Ve Petrolojisi: Amfibolce Zengin Granat Peridotitin Kısmi Ergimesi”. Çukurova Üniversitesi Mühendislik-Mimarlık Fakültesi Dergisi 33/3 (September 2018), 41-56. https://doi.org/10.21605/cukurovaummfd.500540.
JAMA Oyan V. Tutak (Ağrı) Volkanitlerinin Jeokimyası ve Petrolojisi: Amfibolce Zengin Granat Peridotitin Kısmi Ergimesi. cukurovaummfd. 2018;33:41–56.
MLA Oyan, Vural. “Tutak (Ağrı) Volkanitlerinin Jeokimyası Ve Petrolojisi: Amfibolce Zengin Granat Peridotitin Kısmi Ergimesi”. Çukurova Üniversitesi Mühendislik-Mimarlık Fakültesi Dergisi, vol. 33, no. 3, 2018, pp. 41-56, doi:10.21605/cukurovaummfd.500540.
Vancouver Oyan V. Tutak (Ağrı) Volkanitlerinin Jeokimyası ve Petrolojisi: Amfibolce Zengin Granat Peridotitin Kısmi Ergimesi. cukurovaummfd. 2018;33(3):41-56.