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Petrographic And Geochemical Properties Of The Keban Magmatic Rocks (Keban-Elazığ)

Yıl 2021, Cilt: 3 Sayı: 1, 69 - 80, 29.04.2021

Mustafa Eren Rizeli Abdullah Sar Mehmet Ali Ertürk

https://doi.org/10.46387/bjesr.883632
Cited By: 4

Öz

In this study, the petrographic and geochemical characteristics of Late Cretaceous-Middle Eocene Keban magmatic rocks were examined in Keban-Elazığ. Apart from the Keban Magmatic rocks, the other units outcropping around the region are the Late Devonian-Late Triassic Keban Metamorphics, Paleogene-Neogene sedimentary units and Plio-Quaternary alluviums. The investigated rocks are represented by syenite porphyry and quartz-monzonites belonging to Keban Magmatic rocks, which cut the Keban metamorphic rocks. The Keban Magmatic rocks consist of the main minerals are K-feldspar (mega-phenocrystal), plagioclase, amphibole, biotite and quartz minerals, which shows porphyric, porphyric holocrystalline, poikilitic texture in general. All the samples are shoshonitic in composition and fall into the A-type granitoid region. The tectonic environment of the investigated rocks is post-collisional granites.

Anahtar Kelimeler

Keban Magmatic Rocks Petrography Geochemistry Keban Elazığ

Kaynakça

  • [1] B.W. Chappell, A.J.R. White, “I- and S-type granites in the Lachlan Fold Belt. Transactions of the Royal Society of Edinburg”, Earth Sciences, 83, 1-26, 1992.
  • [2] G.N. Eby, “The A-type granitoids: a review of their occurrence and chemical characteristics and speculation on their petrogenesis”, Lithos, 26, 115–134, 1990.
  • [3] M.C. Loiselle, Wones, D.R. “Characteristics and origin of anorogenic granites”, Abstracts Papers to be Presented at the Annual Meetings of the Geological Society of America and Associated Societies, San Diego, CA. 11, p. 468, 1979.
  • [4] J.B. Whalen, K.L. Currie, and B.W. Chappell, “A-type granites: geochemical characteristics, discrimination and petrogenesis”, Contributions to Mineralogy and Petrology, 95, 407–419, 1987.
  • [5] M. Ural, S. Kürüm, “Microscopic and Diffractometric Studies Inferred from Skarn Zonations Between the Keban Metamorphites and Elazığ Magmatites, Around Elazığ”, Turkish Journal of Science & Technology, 4, 2, 87- 102, 2009.
  • [6] L. Kalender, “Oxygen, carbon and sulfur isotope studies in the Keban Pb-Zn deposits, eastern Turkey: an approach on the origin of hydrothermal fluids”, Journal of African Earth Science, 59 (4–5), 341–348, 2011.
  • [7] İ. Kuşçu, R.M. Tosdal, G. Gencalioğlu Kuşcu, R. Friedman, and T.D. Ullrich, “Late Cretaceous to Middle Eocene magmatism and metallogeny of a portion of the Southeastern Anatolian orogenic belt, East-Central Turkey”, Econ. Geology, 108 (4), 641–666, 2013.
  • [8] B. Akgül, “Geochemical associations between fluorite mineralization and A-type shoshonitic magmatism in the Keban Elazig area, East Anatolia, Turkey”, Journal of African Earth Sciences, 111, 222–230, 2015.
  • [9] E. Yıldırım, N. Yıldırım, C. Dönmez, S-M. Koh, and K. Günay, “Mineralogy, rare earth elements geochemistry and genesis of the Keban- West Euphrates (Cu-Mo)-Pb-Zn skarn deposit (Eastern Taurus metallogenic belt, E Turkey)”, Ore Geology Reviews, 114, 103102, 2019.
  • [10] M. Beyarslan, A.F. Bingöl, “Zircon U-Pb age and geochemical constraints on the origin and tectonic implications of late cretaceous intra-oceanic arc magmatics in the Southeast Anatolian Orogenic Belt (SE-Turkey)”, Journal of African Earth Sciences, 147, 477–497, 2018.
  • [11] A. Sar, M.A. Ertürk, and M. Rizeli, “Genesis of Late Cretaceous intra-oceanic arc intrusions in the Pertek area of Tunceli Province, eastern Turkey, and implications for the geodynamic evolution of the southern Neo-Tethys: Results of zircon U–Pb geochronology and geochemical and Sr–Nd isotopic analyses”, Lithos, 350–351, 105263, 2019.
  • [12] T. Rızaoğlu, O. Parlak, V. Hock, F. Koller, W.E. Hames, and Z. Billor, “Andean type active margin formation in the Eastern Taurides: geochemical and geochronological evidence from the Baskil Granitoid, SE Turkey”, Tectonophysics, 473, 188-207, 2009.
  • [13] U.K. Tekin, M. Ural, M.C. Göncüoğlu, M. Arslan, and S. Kürüm, “Upper Cretaceous Radiolarian ages from an arc-back-arc within the Yüksekova Complex in the southern Neotethys mélange, SE Turkey”, Comptes Rendus Palevol, 14, 73–84, 2015.
  • [14] M. Ural, M. Arslan, U.K. Göncüoğlu, and S. Kürüm, “Late Cretaceous arc and back–arc formation within the southern Neotethys: whole–rock, trace element and Sr–Nd–Pb isotopic data from basaltic rocks of the Yüksekova Complex (Malatya– Elazığ, SE Turkey)”, Ofioliti, 40 (1), 57–72, 2015.
  • [15] A. Kaya, “Tectonoestratigraphic reconstruction of the Keban metamorphites based on new fossil findings, Eastern Turkey”, Journal of African Earth Science, 124, 245-257, 2016.
  • [16] N. Özgül, “Torosların bazı temel jeoloji özellikleri”, Turk. Jeol. Kurumu Bul. 19, 65-78,1976.
  • [17] E. Kipman, “Geological and Petrological Features of the Volcanic Rocks in Keban”, Associated Prof. Thesis, Istanbul University, Istanbul, Turkey, pp 200, 1976.
  • [18] E. Yazgan, “Geodynamic evolution of the eastern Taurus region”, In Tekeli, O., Göncüoğlu, M.C. (Eds.), Proceedings of Geology of the Taurus Belt, MTA, Ankara, pp. 199-208, 1984.
  • [19] A.L. Streckeisen, R.W. Le Maitre, “Chemical approximation to modal QAPF classification of the igneous rocks”, Neus Jahrbuch für Mineralogie, 136, 169–206, 1979.
  • [20] E.A.K. Middlemost, “Naming materials in the magma igneous rock system”, Earth Sci. Rev, 37, 215–224, 1994.
  • [21] A. Peccerillo, S.R. Taylor, “Geochemistry of Eocene calcalkaline volcanic rocks from the Kastasmonu area, north Turkey”, Contrib. Miner. Petrol, 58, 63–81, 1976.
  • [22] J.A. Pearce, N.B. Harris, and A.G. Tindle, “Trace elements discrimination diagrams for the tectonic interpretation of granitic rocks”, J. Petrol, 25, 956–983, 1984. [23] B. Cabanis, M. Lecolle, “Le diagramme La/10-Y/ 15-Nb/8: un outfil pour la discrim ination de series volcaniques et la mise en evidence des processus de mélange et/ou de contamination crustale”, Comtes Rendus Academy Sciences, (Ser. II) 309, 2023–2029, 1989.
  • [24] L.L. Zhang, D.C. Zhu, Q. Wang, Z.D. Zhao, D. Liu, and J.C. Xie, “Late Cretaceous volcanic rocks in the Sangri area, southern Lhasa Terrane, Tibet: Evidence for oceanic ridge subduction”, Lithos, 326–327, 144–157, 2019.
  • [25] S.P. Turner, J.D. Foden, and R.S. Morrison, “Derivation of some A-type magmas by fractionation of basaltic magma; an example from the Padthaway Ridge, South Australia”, Lithos, 28, 151–179, 1992.
  • [26] J.H. Yang, F.Y., Wu, S.L. Chung, S.A. Wilde, and M.F. Chu, “A hybrid origin for the Qianshan A-type granite, northeast China: geochemical and Sr–Nd–Hf isotopic evidence”, Lithos, 89, 89–106, 2006.
  • [27] B. Bonin, “A-type granites and related rocks: evolution of a concept problems and prospects”, Lithos, 97, 1–29, 2007.
  • [28] R.A. Creaser, R.C. Price, and R.J. Wormald, “A-type granites revisited: assessment of a residual-source model”, Geology, 19, 163–166, 1991.
  • [29] P.L. King, A.J.R. White, B.W. Chappell, and C.M. Allen, “Characterization and origin of aluminous A-type granites from the Lachlan Fold Belt, southern Australia”, Journal of Petrology, 38, 371–391, 1997.
  • [30] G.N. Eby, “Chemical subdivision of the A-type granitoids: petrogenesis and tectonic implications”, Geology, 20, 641–644. 1992.

Keban Magmatik Kayaçları’nın Petrografik Ve Jeokimyasal Özellikleri (Keban-Elazığ)

Yıl 2021, Cilt: 3 Sayı: 1, 69 - 80, 29.04.2021

Mustafa Eren Rizeli Abdullah Sar Mehmet Ali Ertürk

https://doi.org/10.46387/bjesr.883632
Cited By: 4

Öz

Bu çalışmada, Keban-Elazığ bölgesindeki Geç Kretase-Orta Eosen yaşlı Keban Magmatik kayaçlarının petrografik ve jeokimyasal özellikleri incelenmiştir. Çalışılan bölgede Keban Magmatik Kayaçları dışında Geç Devoniyen-Geç Triyas yaşlı Keban Metamorfitleri, Paleosen-Neojen sedimanter birimleri ve Plio-Kuvaterner yaşlı alüvyonlar yüzeylemektedir. Çalışmanın konusunu oluşturan kayaçlar Keban metamorfik kayaçlarını kesen Keban Magmatik kayaçlarına ait siyenit ve kuvars-monzonitlerle temsil edilmektedir. İncelenen kayaçlar genel olarak porfirik, porfirik holokristalen, poiklitik doku özelliği gösteren K-feldispat (mega-fenokristal), plajiyoklas, amfibol, biyotit ve kuvars mineralleri ana mineral içeriğini oluşturur. İncelenen tüm örnekler şoşonitik karakterli olup A-tipi granitoid alanlarına düşmektedir. İncelenen kayaçların tektonik ortamı olarak çarpışma sonrası granitleri bölgesi önerilmektedir.

Anahtar Kelimeler

Keban Magmatik Kayaçları Petrografi Jeokimya Keban Elazığ

Kaynakça

  • [1] B.W. Chappell, A.J.R. White, “I- and S-type granites in the Lachlan Fold Belt. Transactions of the Royal Society of Edinburg”, Earth Sciences, 83, 1-26, 1992.
  • [2] G.N. Eby, “The A-type granitoids: a review of their occurrence and chemical characteristics and speculation on their petrogenesis”, Lithos, 26, 115–134, 1990.
  • [3] M.C. Loiselle, Wones, D.R. “Characteristics and origin of anorogenic granites”, Abstracts Papers to be Presented at the Annual Meetings of the Geological Society of America and Associated Societies, San Diego, CA. 11, p. 468, 1979.
  • [4] J.B. Whalen, K.L. Currie, and B.W. Chappell, “A-type granites: geochemical characteristics, discrimination and petrogenesis”, Contributions to Mineralogy and Petrology, 95, 407–419, 1987.
  • [5] M. Ural, S. Kürüm, “Microscopic and Diffractometric Studies Inferred from Skarn Zonations Between the Keban Metamorphites and Elazığ Magmatites, Around Elazığ”, Turkish Journal of Science & Technology, 4, 2, 87- 102, 2009.
  • [6] L. Kalender, “Oxygen, carbon and sulfur isotope studies in the Keban Pb-Zn deposits, eastern Turkey: an approach on the origin of hydrothermal fluids”, Journal of African Earth Science, 59 (4–5), 341–348, 2011.
  • [7] İ. Kuşçu, R.M. Tosdal, G. Gencalioğlu Kuşcu, R. Friedman, and T.D. Ullrich, “Late Cretaceous to Middle Eocene magmatism and metallogeny of a portion of the Southeastern Anatolian orogenic belt, East-Central Turkey”, Econ. Geology, 108 (4), 641–666, 2013.
  • [8] B. Akgül, “Geochemical associations between fluorite mineralization and A-type shoshonitic magmatism in the Keban Elazig area, East Anatolia, Turkey”, Journal of African Earth Sciences, 111, 222–230, 2015.
  • [9] E. Yıldırım, N. Yıldırım, C. Dönmez, S-M. Koh, and K. Günay, “Mineralogy, rare earth elements geochemistry and genesis of the Keban- West Euphrates (Cu-Mo)-Pb-Zn skarn deposit (Eastern Taurus metallogenic belt, E Turkey)”, Ore Geology Reviews, 114, 103102, 2019.
  • [10] M. Beyarslan, A.F. Bingöl, “Zircon U-Pb age and geochemical constraints on the origin and tectonic implications of late cretaceous intra-oceanic arc magmatics in the Southeast Anatolian Orogenic Belt (SE-Turkey)”, Journal of African Earth Sciences, 147, 477–497, 2018.
  • [11] A. Sar, M.A. Ertürk, and M. Rizeli, “Genesis of Late Cretaceous intra-oceanic arc intrusions in the Pertek area of Tunceli Province, eastern Turkey, and implications for the geodynamic evolution of the southern Neo-Tethys: Results of zircon U–Pb geochronology and geochemical and Sr–Nd isotopic analyses”, Lithos, 350–351, 105263, 2019.
  • [12] T. Rızaoğlu, O. Parlak, V. Hock, F. Koller, W.E. Hames, and Z. Billor, “Andean type active margin formation in the Eastern Taurides: geochemical and geochronological evidence from the Baskil Granitoid, SE Turkey”, Tectonophysics, 473, 188-207, 2009.
  • [13] U.K. Tekin, M. Ural, M.C. Göncüoğlu, M. Arslan, and S. Kürüm, “Upper Cretaceous Radiolarian ages from an arc-back-arc within the Yüksekova Complex in the southern Neotethys mélange, SE Turkey”, Comptes Rendus Palevol, 14, 73–84, 2015.
  • [14] M. Ural, M. Arslan, U.K. Göncüoğlu, and S. Kürüm, “Late Cretaceous arc and back–arc formation within the southern Neotethys: whole–rock, trace element and Sr–Nd–Pb isotopic data from basaltic rocks of the Yüksekova Complex (Malatya– Elazığ, SE Turkey)”, Ofioliti, 40 (1), 57–72, 2015.
  • [15] A. Kaya, “Tectonoestratigraphic reconstruction of the Keban metamorphites based on new fossil findings, Eastern Turkey”, Journal of African Earth Science, 124, 245-257, 2016.
  • [16] N. Özgül, “Torosların bazı temel jeoloji özellikleri”, Turk. Jeol. Kurumu Bul. 19, 65-78,1976.
  • [17] E. Kipman, “Geological and Petrological Features of the Volcanic Rocks in Keban”, Associated Prof. Thesis, Istanbul University, Istanbul, Turkey, pp 200, 1976.
  • [18] E. Yazgan, “Geodynamic evolution of the eastern Taurus region”, In Tekeli, O., Göncüoğlu, M.C. (Eds.), Proceedings of Geology of the Taurus Belt, MTA, Ankara, pp. 199-208, 1984.
  • [19] A.L. Streckeisen, R.W. Le Maitre, “Chemical approximation to modal QAPF classification of the igneous rocks”, Neus Jahrbuch für Mineralogie, 136, 169–206, 1979.
  • [20] E.A.K. Middlemost, “Naming materials in the magma igneous rock system”, Earth Sci. Rev, 37, 215–224, 1994.
  • [21] A. Peccerillo, S.R. Taylor, “Geochemistry of Eocene calcalkaline volcanic rocks from the Kastasmonu area, north Turkey”, Contrib. Miner. Petrol, 58, 63–81, 1976.
  • [22] J.A. Pearce, N.B. Harris, and A.G. Tindle, “Trace elements discrimination diagrams for the tectonic interpretation of granitic rocks”, J. Petrol, 25, 956–983, 1984. [23] B. Cabanis, M. Lecolle, “Le diagramme La/10-Y/ 15-Nb/8: un outfil pour la discrim ination de series volcaniques et la mise en evidence des processus de mélange et/ou de contamination crustale”, Comtes Rendus Academy Sciences, (Ser. II) 309, 2023–2029, 1989.
  • [24] L.L. Zhang, D.C. Zhu, Q. Wang, Z.D. Zhao, D. Liu, and J.C. Xie, “Late Cretaceous volcanic rocks in the Sangri area, southern Lhasa Terrane, Tibet: Evidence for oceanic ridge subduction”, Lithos, 326–327, 144–157, 2019.
  • [25] S.P. Turner, J.D. Foden, and R.S. Morrison, “Derivation of some A-type magmas by fractionation of basaltic magma; an example from the Padthaway Ridge, South Australia”, Lithos, 28, 151–179, 1992.
  • [26] J.H. Yang, F.Y., Wu, S.L. Chung, S.A. Wilde, and M.F. Chu, “A hybrid origin for the Qianshan A-type granite, northeast China: geochemical and Sr–Nd–Hf isotopic evidence”, Lithos, 89, 89–106, 2006.
  • [27] B. Bonin, “A-type granites and related rocks: evolution of a concept problems and prospects”, Lithos, 97, 1–29, 2007.
  • [28] R.A. Creaser, R.C. Price, and R.J. Wormald, “A-type granites revisited: assessment of a residual-source model”, Geology, 19, 163–166, 1991.
  • [29] P.L. King, A.J.R. White, B.W. Chappell, and C.M. Allen, “Characterization and origin of aluminous A-type granites from the Lachlan Fold Belt, southern Australia”, Journal of Petrology, 38, 371–391, 1997.
  • [30] G.N. Eby, “Chemical subdivision of the A-type granitoids: petrogenesis and tectonic implications”, Geology, 20, 641–644. 1992.
Toplam 29 adet kaynakça vardır.

Ayrıntılar

Birincil Dil Türkçe
Konular Yer Bilimleri ve Jeoloji Mühendisliği (Diğer)
Bölüm Araştırma Makaleleri
Yazarlar

Mustafa Eren Rizeli 0000-0003-3725-3063

Abdullah Sar 0000-0002-9752-7807

Mehmet Ali Ertürk 0000-0003-1197-9202

Yayımlanma Tarihi 29 Nisan 2021
Yayımlandığı Sayı Yıl 2021 Cilt: 3 Sayı: 1

Kaynak Göster

APA Rizeli, M. E., Sar, A., & Ertürk, M. A. (2021). Keban Magmatik Kayaçları’nın Petrografik Ve Jeokimyasal Özellikleri (Keban-Elazığ). Mühendislik Bilimleri Ve Araştırmaları Dergisi, 3(1), 69-80. https://doi.org/10.46387/bjesr.883632
AMA Rizeli ME, Sar A, Ertürk MA. Keban Magmatik Kayaçları’nın Petrografik Ve Jeokimyasal Özellikleri (Keban-Elazığ). Müh.Bil.ve Araş.Dergisi. Nisan 2021;3(1):69-80. doi:10.46387/bjesr.883632
Chicago Rizeli, Mustafa Eren, Abdullah Sar, ve Mehmet Ali Ertürk. “Keban Magmatik Kayaçları’nın Petrografik Ve Jeokimyasal Özellikleri (Keban-Elazığ)”. Mühendislik Bilimleri Ve Araştırmaları Dergisi 3, sy. 1 (Nisan 2021): 69-80. https://doi.org/10.46387/bjesr.883632.
EndNote Rizeli ME, Sar A, Ertürk MA (01 Nisan 2021) Keban Magmatik Kayaçları’nın Petrografik Ve Jeokimyasal Özellikleri (Keban-Elazığ). Mühendislik Bilimleri ve Araştırmaları Dergisi 3 1 69–80.
IEEE M. E. Rizeli, A. Sar, ve M. A. Ertürk, “Keban Magmatik Kayaçları’nın Petrografik Ve Jeokimyasal Özellikleri (Keban-Elazığ)”, Müh.Bil.ve Araş.Dergisi, c. 3, sy. 1, ss. 69–80, 2021, doi: 10.46387/bjesr.883632.
ISNAD Rizeli, Mustafa Eren vd. “Keban Magmatik Kayaçları’nın Petrografik Ve Jeokimyasal Özellikleri (Keban-Elazığ)”. Mühendislik Bilimleri ve Araştırmaları Dergisi 3/1 (Nisan 2021), 69-80. https://doi.org/10.46387/bjesr.883632.
JAMA Rizeli ME, Sar A, Ertürk MA. Keban Magmatik Kayaçları’nın Petrografik Ve Jeokimyasal Özellikleri (Keban-Elazığ). Müh.Bil.ve Araş.Dergisi. 2021;3:69–80.
MLA Rizeli, Mustafa Eren vd. “Keban Magmatik Kayaçları’nın Petrografik Ve Jeokimyasal Özellikleri (Keban-Elazığ)”. Mühendislik Bilimleri Ve Araştırmaları Dergisi, c. 3, sy. 1, 2021, ss. 69-80, doi:10.46387/bjesr.883632.
Vancouver Rizeli ME, Sar A, Ertürk MA. Keban Magmatik Kayaçları’nın Petrografik Ve Jeokimyasal Özellikleri (Keban-Elazığ). Müh.Bil.ve Araş.Dergisi. 2021;3(1):69-80.

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