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Çarpışma Sonrası Pliyo-Kuvaterner Gözucu (Taşlıçay-Ağrı) Volkaniklerinin Jeokimyasal Özellikleri ve Magma Kaynak Bölge Karakteristikleri, Doğu Anadolu, Türkiye

Year 2020, Volume: 63 Issue: 2, 195 - 214, 10.02.2020
https://doi.org/10.25288/tjb.569247

Abstract

Bu çalışma Pliyo-Kuvaterner yaşlı Gözucu (Taşlıçay-Ağrı) volkaniklerinin petrografik ve jeokimyasal özelliklerinin belirlenmesini amaçlar. İncelenen volkanikler subalkali, kalkalkali, yüksek K’lu seri ve şoşonitik özelliklere sahip olup, bazalt, andezit, trakiandezit, trakidasit ve dasitlerden meydana gelirler. Gözucu volkanikleri hafif nadir toprak elementleri (HNTE) ve büyük iyonlu litofil elementlerde (BİLE) zenginleşme, ağır nadir toprak elementleri (ANTE) ve kalıcılığı yüksek elementlerde (KYE) tüketilmeye sahiptirler. Gözucu volkanikleri kıtasal kabuğun ortalama Sr ve Ba değerlerine yakın Sr ve Ba değerlerine (Sr-379 ppm Ba-639 ppm) sahiptirler. Bu yüksek değerler Gözucu volkaniklerinin oluşumu sırasında kıtasal kabuk kayaçlarından kirlenmeye uğradığına işaret eder. Düşük Nb/La (5,13 ppm) ve yüksek Ba/Rb (16,75 ppm) oranı Gözucu volkaniklerinin kirlenme süreci sırasında akışkanlardan ziyade sediment katkısının daha baskın rol oynadığını ifade etmektedir. Ana ve eser elementlerin ikili değişim diyagramlarındaki artma ve azalma eğilimleri fraksiyonel kristallenmeye ve tek bir manto kaynağına işaret etmektedir. Jeodinamik ortam olarak kıtasal yay ortamında ve çarpışma sonrasında oluşmuştur. Gözucu volkanikleri spinel mineralojisi açısından zengin bir litosferik manto kaynak bölgesinin %0,1 ile %3 oranında kısmi erimesi sonucu oluşmuştur. 

Supporting Institution

Van Yüzüncü Yıl Üniversitesi Bilimsel Araştırma Projeleri Başkanlığı

Project Number

2010-FBE-YL 145

References

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Geochemical Features and Magma Source Regional Characteristics of the Post-Collisional Plio-Quaternary Gözucu (Taşlıçay-Ağrı) Volcanics, Eastern Anatolia, Turkey

Year 2020, Volume: 63 Issue: 2, 195 - 214, 10.02.2020
https://doi.org/10.25288/tjb.569247

Abstract

This study aimed to determine the petrographic and geochemical features of the Plio-Quaternary Gözucu (Taşlıçay-Ağrı) volcanics. These volcanics have subalkaline, calc-alkaline, high-K-series and shoshonitic features and are composed of basalt, andesite, trachyandesite, trachydacite and dacites. The Gözucu volcanics exhibit enrichment in light rare earth elements (LREE) and large ion lithophile elements (LILE) while showing depletion in heavy rare earth elements (HREE) and high field strength elements (HFSE). The average Sr and Ba values of Gözucu volcanics are close to continental crust values (Sr-379 ppm Ba-639 ppm), which means that these rocks were contaminated by the continental crust during formation. Low Nb/La (5.13 ppm) and high Ba/Rb (16.75 ppm) ratios indicate that the contribution of sediments was more than that of fluids during the contamination process of the Gözucu volcanics. Positive and negative trends of major and trace elements in the variation diagrams indicate fractional crystallization and a single mantle source. The Gözucu volcanics occurred with a partial melting of the spinel-rich lithospheric mantle source with 0.1-3% partial melting in the continental arc environment after the collision.

Project Number

2010-FBE-YL 145

References

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  • Açlan, M., Turgut, İ.K. 2017. Şekerbulak (Diyadin-Ağrı) Dolaylarında Yüzeyleyen Volkanik Kayaçların Mineralojik-Petrografik ve Jeokimyasal Özellikleri Çukurova Üniversitesi Mühendislik ve Mimarlık Fakültesi Dergisi, 32 (4), 163-174.
  • Açlan, M., Altun, Y. 2018. Syn-collisional I-type Esenköy Pluton (Eastern Anatolia-Turkey): An indication for collision between Arabian and Eurasian plates. Journal of African Earth Sciences, 142, 1-11.
  • Açlan, M., Duruk, H.İ. 2018. Geochemistry, zircon U-Pb geochronology and tectonic setting of the Taşlıçay Granitoids, Eastern Anatolia, Turkey. Arabian Journal of Geosciences, 11 (336), 1-19.
  • Açlan, M., Davran, N. 2019. Karlıca Volkanitlerinin (Hamur-Ağrı) Petrografik ve Jeokimyasal Özellikleri. Hacettepe Üniversitesi Yerbilimleri Uygulama ve Araştırma Merkezi Bülteni, 40 (1), 72-91.
  • Al-Lazki, A., Seber, D., Sandvol, E., Türkelli, N., Mohamad, R., Barazangi, M. 2003. Tomographic Pn velocity and anisotropy structure beneath the Anatolian plateau (Eastern Turkey) and the surrounding regions. Geophysical Research Letters, 30, 8043.
  • Altun, Y. 2016. Oğlaklı-Gözucu (Taşlıçay-Ağrı) Dolaylarında Yüzeyleyen Kayaçların Mineralojik-Petrografik İncelenmesi. Van Yüzüncü Yıl Üniversitesi Fen Bilimleri Enstitüsü Yüksek Lisans Tezi, 141 s., (yayınlanmamış).
  • Alvarado, A., Audin, L., Nocquet, J.M., Lagreulet, S., Segovia Font, Y., Lamarque, G., Yepes, H., Mothes, P., Rolandone, F., Jarrin, P., Quidelleur, X. 2014. Active tectonics in Quito, Ecuador, assessed by geomorphological studies, GPS data, and crustal seismicity. Tectonics, 33, 67-83.
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  • Ayalew, D., Barbey, P., Marty, B., Reisberg, L., Yirgu, G., Pik, R. 2002. Source, genesis, and timing of giant ignimbrite deposits associated with Ethiopian continental flood basalts. Geochimica Cosmochimica Acta, 66 (8), 1429–1448.
  • Ayalew, D., Gibson, S.A. 2009. Head-to-tail transition of the Afar mantle plume: geochemical evidence from a Miocene bimodal basalt–rhyolite succession in the Ethiopian Large Igneous Province. Lithos, 112 (3), 461–476.
  • Azzone, R.G., Munoz, P.M., Enrich, G.E., Alves, A., Ruberti, E., Gomes, C.B., 2016. Petrographic, geochemical and isotopic evidence of crustal assimilation processes in the Ponte Nova alkaline mafic-ultramafic massif, SE Brazil. Lithos, 260, 58–75.
  • Barazangi, M., Sandvol, E., Seber, D. 2006. Structure and tectonic evolution of the Anatolian Plateau in eastern Turkey, (Postcollisional Tectonics and Magmatism in the Mediterranean Region and Asia, Editörler: Dilek, Y., Pavlides, S.). Geological Society of America Special Paper, 409, 463–473.
  • Beard, J.S., Ragland, P.C., Crawford, M.L. 2005. Reactive bulk assimilation: A model for crust-mantle mixing in silicic magmas. Geology, 33 (8), 681–684.
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There are 80 citations in total.

Details

Primary Language Turkish
Subjects Geological Sciences and Engineering (Other)
Journal Section Makaleler - Articles
Authors

Mustafa Açlan 0000-0002-2131-8646

Yusuf Altun This is me 0000-0002-1963-8149

Project Number 2010-FBE-YL 145
Publication Date February 10, 2020
Submission Date May 23, 2019
Acceptance Date September 16, 2019
Published in Issue Year 2020 Volume: 63 Issue: 2

Cite

APA Açlan, M., & Altun, Y. (2020). Çarpışma Sonrası Pliyo-Kuvaterner Gözucu (Taşlıçay-Ağrı) Volkaniklerinin Jeokimyasal Özellikleri ve Magma Kaynak Bölge Karakteristikleri, Doğu Anadolu, Türkiye. Türkiye Jeoloji Bülteni, 63(2), 195-214. https://doi.org/10.25288/tjb.569247
AMA Açlan M, Altun Y. Çarpışma Sonrası Pliyo-Kuvaterner Gözucu (Taşlıçay-Ağrı) Volkaniklerinin Jeokimyasal Özellikleri ve Magma Kaynak Bölge Karakteristikleri, Doğu Anadolu, Türkiye. Geol. Bull. Turkey. March 2020;63(2):195-214. doi:10.25288/tjb.569247
Chicago Açlan, Mustafa, and Yusuf Altun. “Çarpışma Sonrası Pliyo-Kuvaterner Gözucu (Taşlıçay-Ağrı) Volkaniklerinin Jeokimyasal Özellikleri Ve Magma Kaynak Bölge Karakteristikleri, Doğu Anadolu, Türkiye”. Türkiye Jeoloji Bülteni 63, no. 2 (March 2020): 195-214. https://doi.org/10.25288/tjb.569247.
EndNote Açlan M, Altun Y (March 1, 2020) Çarpışma Sonrası Pliyo-Kuvaterner Gözucu (Taşlıçay-Ağrı) Volkaniklerinin Jeokimyasal Özellikleri ve Magma Kaynak Bölge Karakteristikleri, Doğu Anadolu, Türkiye. Türkiye Jeoloji Bülteni 63 2 195–214.
IEEE M. Açlan and Y. Altun, “Çarpışma Sonrası Pliyo-Kuvaterner Gözucu (Taşlıçay-Ağrı) Volkaniklerinin Jeokimyasal Özellikleri ve Magma Kaynak Bölge Karakteristikleri, Doğu Anadolu, Türkiye”, Geol. Bull. Turkey, vol. 63, no. 2, pp. 195–214, 2020, doi: 10.25288/tjb.569247.
ISNAD Açlan, Mustafa - Altun, Yusuf. “Çarpışma Sonrası Pliyo-Kuvaterner Gözucu (Taşlıçay-Ağrı) Volkaniklerinin Jeokimyasal Özellikleri Ve Magma Kaynak Bölge Karakteristikleri, Doğu Anadolu, Türkiye”. Türkiye Jeoloji Bülteni 63/2 (March 2020), 195-214. https://doi.org/10.25288/tjb.569247.
JAMA Açlan M, Altun Y. Çarpışma Sonrası Pliyo-Kuvaterner Gözucu (Taşlıçay-Ağrı) Volkaniklerinin Jeokimyasal Özellikleri ve Magma Kaynak Bölge Karakteristikleri, Doğu Anadolu, Türkiye. Geol. Bull. Turkey. 2020;63:195–214.
MLA Açlan, Mustafa and Yusuf Altun. “Çarpışma Sonrası Pliyo-Kuvaterner Gözucu (Taşlıçay-Ağrı) Volkaniklerinin Jeokimyasal Özellikleri Ve Magma Kaynak Bölge Karakteristikleri, Doğu Anadolu, Türkiye”. Türkiye Jeoloji Bülteni, vol. 63, no. 2, 2020, pp. 195-14, doi:10.25288/tjb.569247.
Vancouver Açlan M, Altun Y. Çarpışma Sonrası Pliyo-Kuvaterner Gözucu (Taşlıçay-Ağrı) Volkaniklerinin Jeokimyasal Özellikleri ve Magma Kaynak Bölge Karakteristikleri, Doğu Anadolu, Türkiye. Geol. Bull. Turkey. 2020;63(2):195-214.

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