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Doğu Anadolu Fay Sistemi Boyunca Gelişen Kuvaterner Mafik Alkali Volkanizmasının Petrojenezi ve Tektonik Konumu, Güneydoğu Anadolu Orojenik Kuşağı (Elazığ)

Yıl 2022, Cilt: 9 Sayı: 1, 171 - 188, 31.01.2022
https://doi.org/10.31202/ecjse.955277

Öz

Bu çalışma ile Elazığ Bölgesinde yüzeyleyen Kuvaterner volkanik kayaçlarının inceleme sonuçları verilmiştir. Sol yönlü doğrultu atımlı Doğu Anadolu Fay Zonu (EAFZ) Türkiye’nin en önemli faylarından birisidir. Elazığ bölgesinde EAFZ boyunca mafik alkali özellikte volkanik kayaçlar yüzeylemektedir. Bu volkanik kayaçlar, yüksek LILE ve HFSE içeriklerine ve düşük LILE/HFSE oranlarına (Ba/Nb=2.28-10.7) ve düşük 87Sr/86Sr (0.703149-0.703915) ve yüksek 143Nd/144Nd (0.512751-0.512895) oranlarına sahiptirler. Kimyasal bileşimleri levha içi magmaların bileşimlerine benzemektedirler. Yüksek Nb (34-76.6 ppm), ve Nb/La oranları (>1.0) gösterirler. Nb/La oranları lavların kirlenmemiş veya çok az kirlenmiş olduğunu belirtmektedir. Pozitif Sr anomalisi ve Eu anomalisinin olmaması plajiyoklasların esas fraksiyonlaşma mineral fazı olmadığını belirtir. Farklı veriler Harput volkanitlerinin spinel lerzolitin düşük derecede kısmi ergimesi (~%0.4-4) ile Doğu Anadolu Fay Zonu’na ait fay sistemlerinin kesişme noktalarında oluşmuştur.

Teşekkür

Bu çalışma, 1980 yılından bu yana farklı zamanlarda Fırat Üniversitesi Bilimsel Araştırma Projeleri (FÜBAP) ile desteklenmiştir. Bu çalışmanın ortaya çıkmasında verdiği destekten ötürü Bilimsel Araştırma Projeleri Birimine teşekkür ederiz.

Kaynakça

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Petrogenesis and Tectonic Setting of the Quaternary Mafic Alkaline Volcanism Along with the East Anatolian Fault System, Southeastern Anatolia Orogenic Belt (Elazığ)

Yıl 2022, Cilt: 9 Sayı: 1, 171 - 188, 31.01.2022
https://doi.org/10.31202/ecjse.955277

Öz

We report the results of a study on Quaternary volcanic rocks cropping out in the Elazığ region. Here the sinistral transform East Anatolian Fault Zone (EAFZ) is one of the important strike-slip faults of Turkey. The Harput mafic alkaline lavas erupted along with strike-slip fault systems in the Elazığ region in southern Turkey. The Quaternary alkali basalts have higher LILE and HFSE contents and lower LILE/HFSE ratios (Ba/Nb = 2.28-10.7), low 87Sr/86Sr (0.703149-0.703915) and high 143Nd/144Nd (0.512751-0.512895), with compositions similar to those of intraplate magmas. They have high Nb contents (34-76.6 ppm), and Nb/La ratios (>1.0). The Nb/La ratios indicate that the lavas are uncontaminated. The positive Sr anomalies and the lack of Eu anomalies imply that plagioclase was not a major fractionating mineral phase. The different data of the Harput volcanics indicate that the volcanism formed at the intersections of the fault systems that belong to the EAFZ and were produced by the lower degree of partial melting (~0.4-4%) of spinel lherzolite.

Kaynakça

  • [1]. Glazner, A.F., “Plutonism, oblique subduction, and continental growth: An example from the Mesozoic of California”, Geology, 1991, 19, 784–786.
  • [2]. Hamilton, W.B., “Subduction systems and magmatism. In: Smellie JR (Ed.), Volcanis Associated with Extension to Consuming Plate Margins”, Geol Soc London Spec Publ., 1995, 81, 3–28.
  • [3]. Watanabe, T., Koyaguchi, T., Seno, T., “Tectonic stress controls on ascent and emplacement of magmas”, J.Volcanol Geotherm Res. 1999, 91, 65–78.
  • [4]. Williams, H., McBirney, A.,. Volcanology, Freeman, Cooper and Co., 1979.
  • [5]. Nakamura, K., “Volcanoes as possible indicators of tectonic stress orientation: principle and proposal”, J.Volcanol Geotherm Res., 1977, 2, 1–16.
  • [6]. White, R., McKenzie, D., “Magmatism at rift zones: The generation of volcanic continental margins and flood basalts”, J. Geophys. Res., 1989, 94, 7685-7729. [7]. Hoffman, A.W., “Mantle geochemistry: the message from oceanic volcanism”, Nature, 1997, 385, 219–229.
  • [8]. Valentine, G.A., Perry, F.V., Krier, D., Keating, G.N., Kelley, R.E., Cogbill, A.H., “Small volume basaltic volcanoes: eruptive products and processes, and posteruptive geomorphic evolution in Crater Flat (Pleistocene), southern Nevada”, Geol. Soc. Am. Bull., 2006, 118, 1313–1330.
  • [9]. Arger, J., Mitchell, J.G., Westaway, R.W.C., “Neogene and Quaternary volcanism of southeastern Turkey”. In: Bozkurt, E., Winchester, J.A., Piper, J.D.A. (Eds.), Tectonics and Magmatism in Turkey and its Surrounding Area. Geological Society, London, 2000,pp. 459–487.
  • [10]. Keskin, M., “Eastern Anatolia: a hot spot in a collision zone without a mantle pluma”, (Plates, Plumes and Planetary Processes, Editörler: Foulger, G.R., Jurdy, D.). Geological Society of America Special Papers, 2007, 430, 693-722.
  • [11]. Ekici, T., Alpaslan, M., Parlak, Temel, A., “Geochemistry of the Pliocene basalts erupted along the Malatya-Ovacık fault zone (MOFZ), eastern Anatolia, Turkey: implications for source characteristics and partial melting processes”, Chemie der Erde, 2007, 67, 201-212.
  • [12]. Kocaarslan, A., Ersoy, E. Y., “Petrologic evolution of Miocene‐Pliocene mafic volcanism in the Kangal and Gürün basins (Sivas‐Malatya), central east Anatolia: Evidence for Miocene anorogenic magmas contaminated by continental crust”, 2018, Lithos, 310, 392-408.
  • [13]. Di Giuseppe, P., Agostini, S., Lustrino, M., Karaoğlu, Ö., Savaşçın, M.Y., Manetti, P., Ersoy, Y., “Transition from Compression to Strike-slip Tectonics Revealed by Miocene–Pleistocene Volcanism West of the Karlıova Triple Junction (East Anatolia)”, 2017, 58, 10, 2055-2087.
  • [14]. Naz, H., “Elazığ-Palu dolayının jeolojisi” TPAO, raport No: 1360, Ankara (Unpublished), 1979.
  • [15]. Kara, H., Bal Akkoca, D., “Doğanşehir (Malatya)’da ki Barit Cevherleşmelerinin Kökeni: İz ve Nadir Toprak Element, İzotop ve Sıvı Kapanım Bulguları” El-Cezerî Fen ve Mühendislik Dergisi, 2021, 8 (2); 1035-1050.
  • [16]. Rojay, B., Heimann, A., Toprak, V., “Neotectonic and volcanic characteristics of the Karasu fault zone (Anatolia, Turkey): The transition zone between the Dead Sea transform and the East Anatolian fault zone”, Geodinamica Acta. Vol., 2001. 14, 1–3, 197-212.
  • [17]. Dewey, F.J., Hempton, M.R., Kidd, W.S.F., Saroğlu, F., Şengör, A.M.C., “Shortening of continental lithosphere: the neotectonics of Eastern Anatolia—a young collision zone. In: Coward, M. P. & Ries, A. C. (eds) Collision Tectonics”, Geological Society. London. Special Publications. Vol., 1986, 19, 1–36.
  • [18]. Barka, A.A., Cadinsky-Cade, K., “Strike-slip fault geometry in Turkey and its influence on earthquake activity”, Tectonics, 1988, 7 (3), 663–684.
  • [19]. Bingöl, A.F., “Geology of the Elazıg area in the Eastern Taurus region”. In: Tekeli, O., Göncüoğlu, M.C. (Eds.), International Symposium on the Geology of the Taurus Belt, pp. 26–29 September, MTA, Ankara, 1984, 209-216.
  • [20]. Kaya, A., “Tectono-stratigraphic reconstruction of the Keban metamorphites based on new fossil findings, Eastern Turkey”, Journal of African Earth Sciences, 2016, 124, 245-257.
  • [21]. Demirtaşlı, E., “Pınarbaşı-Sarız-Mağara civarının jeoloji raporu”, MTA Report No: 1935. Ankara, Turkey (in Turkish), 1967.
  • [22]. Beyarslan, M., Bingöl, A.F., “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, 2018, 147, 477–497.
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Toplam 68 adet kaynakça vardır.

Ayrıntılar

Birincil Dil Türkçe
Konular Mühendislik
Bölüm Makaleler
Yazarlar

Melahat Beyarslan 0000-0002-1309-9834

Mehmet Ali Ertürk 0000-0003-1197-9202

Mustafa Eren Rizeli 0000-0003-3725-3063

Abdullah Sar 0000-0002-9752-7807

Yayımlanma Tarihi 31 Ocak 2022
Gönderilme Tarihi 21 Haziran 2021
Kabul Tarihi 5 Ekim 2021
Yayımlandığı Sayı Yıl 2022 Cilt: 9 Sayı: 1

Kaynak Göster

IEEE M. Beyarslan, M. A. Ertürk, M. E. Rizeli, ve A. Sar, “Doğu Anadolu Fay Sistemi Boyunca Gelişen Kuvaterner Mafik Alkali Volkanizmasının Petrojenezi ve Tektonik Konumu, Güneydoğu Anadolu Orojenik Kuşağı (Elazığ)”, ECJSE, c. 9, sy. 1, ss. 171–188, 2022, doi: 10.31202/ecjse.955277.