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Petrologic Evolution of Post-collisional Magmas of Spinel-lherzolite Subcontinental Mantle Contaminated by Continental Crust; Palandöken (Erzurum) Volcanic Rocks in the East Anatolia, Turkey

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Journal of the Geological Society of India

Abstract

The Palandöken volcanics are made up of a thick volcanic sequence consisting dominantly of tuffs and intercalated lava flows in Erzurum-Tekman basin. According to the data obtained from geochemical analyses, the silica contents of the lavas range from 47.44 % (basalt) to 67.68 % (dacite) and Mg# 11–53%. While alkaline (latite and benmoreite) and subalkaline lavas are generally enriched in large ion lithophile elements (LILE) and light rare earth elements (LREE) in conformity with each other, they show significant negative Nb, Ta anomalies and very weak Eu anomaly. There are also examples (N15, N19) in these rocks that differ in their elements behavior. These geochemical characteristics indicate that, starting from the source magma, various differentiation processes like magma mixing and melt effect, occurred. Whereas the Nd (143Nd/144Ndi) isotope values of the volcanic rocks vary in a narrow range of 0.51281 and 0.51267, Sr isotope (87Sr/86Sri) values have a relatively wider range between 0.70362 and 0.70500, and εNd(t) values (+0.71 to +5.14). Isotope and geochemical data; supports that these volcanics were formed by the partial melting of spinel-lherzolite subcontinental lithospheric mantle-derived magma at different rates, but assimilation of continental crust also played an important role, along with magma mixing and fractional crystallization, which constitute the main differentiation process.

Palandöken volcanic rocks have similar geochemical characteristics with the nearby Ilica, Kandilli and Yolçatý volcanics in general and their properties are compatible with eastern Anatolian magmatism that was formed in a geodynamic setting of post-collisional extension.

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Acknowledgements

The authors would like to thank the University of Firat Scientific Research Projects Unit (FÜBAP) for research support (Project number MF-16. 45).

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  1. Department of Geology, Engineering Faculty, University of Firat, Elazig, Turkey

    S. Kürüm & A. Sar

  2. Institute of Science and Technology, University of Firat, Elazig, Turkey

    N. Nas

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Kürüm, S., Sar, A. & Nas, N. Petrologic Evolution of Post-collisional Magmas of Spinel-lherzolite Subcontinental Mantle Contaminated by Continental Crust; Palandöken (Erzurum) Volcanic Rocks in the East Anatolia, Turkey. J Geol Soc India 99, 23–36 (2023). https://doi.org/10.1007/s12594-023-2263-7

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