Petrographic and geochemical characteristics of Late Cretaceous volcanic rocks in the vicinity of Avliyana (Gümüşhane, NE Turkey)
Keywords:
Eastern pontides, Gümüşhane, late cretaceous, whole-rock geochemistry, petrography, Avliyana volcanic rocks
Abstract
In this study, the Late Cretaceous volcanic rocks outcropping in Avliyana (Gümüşhane-NE Turkey) and its surroundings in the Southern Zone of the Eastern Pontides were investigated as petrographically and geochemically. The Late Cretaceous Avliyana volcanic rocks are basalt, basaltic andesite and andesite in composition, and are mainly composed of plagioclase, alkali feldspar, hornblende, biotite and minor augite minerals. Volcanic rocks have calc-alkaline character and have low to high-K content. They are enriched with large ion lithophile elements (LILEs) and light rare earth elements (LREEs) and depleted in terms of elements with high-field strenght elements (HFSEs). The chondrite-normalized rare earth element distributions are concave with low to moderate enrichment (LaN/LuN=3-12), indicating that the volcanic rocks originated from the same source. Fractional crystallization and a lesser assimilation played an impotant role in the development of volcanic rocks. All these data indicate that the studied volcanic rocks were possibly derived from the partial melting of a subcontinental lithospheric mantle (SCLM), which was enriched by fluids and/or sediments from a subduction of oceanic crust.
References
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[4] Vural A, Kaygusuz A. Petrology of the Paleozoic Plutons in Eastern Pontides: Artabel Pluton (Gümüşhane, NE Turkey). Journal of Engineering Research and Applied Science 2019; 8:1216–1228.
[5] Temizel İ, Arslan M, Yücel C, Yazar EA, Kaygusuz A, Aslan Z. U-Pb geochronology, bulk-rock geochemistry and petrology of Late Cretaceous syenitic plutons in the Gölköy (Ordu) area (NE Turkey): Implications for magma generation in a continental arc extension triggered by slab roll-back. Journal of Asian Earth Sciences 2019; 171:305–320.
[6] Temizel I, Arslan M, Yücel C, Abdioğlu Yazar E, Kaygusuz A, Aslan Z. Eocene tonalite–granodiorite from the Havza (Samsun) area, northern Turkey: adakite-like melts of lithospheric mantle and crust generated in a post-collisional setting. International Geology Review 2020; 62:1131–1158.
[7] Sipahi F, Saydam Eker Ç, Akpınar İ, Gücer MA, Vural A, Kaygusuz A, Aydurmuş T. Eocene magmatism and associated Fe-Cu mineralization in northeastern Turkey: a case study of the Karadağ skarn. International Geology Review 2021:1–26.
[8] Vural A, Akpınar İ, Kaygusuz A, Sipahi F. Petrological characteristics of Eocene volcanic rocks around Demirören (Gümüşhane, NE Turkey). Journal of Engineering Research and Applied Science 2021; 10:1703–1716.
[9] Kaygusuz A, Arslan M, Sipahi F, Temizel İ. U-Pb zircon chronology and petrogenesis of Carboniferous plutons in the northern part of the Eastern Pontides, NE Turkey: Constraints for Paleozoic magmatism and geodynamic evolution. Gondwana Research 2016; 39:327–346.
[10] Çamur MZ, Güven İH, Er M. Geochemical characteristics of the eastern Pontide volcanics: an example of multiple volcanic cycles in arc evolution. Turkish Journal of Earth Sciences 1996:123–144.
[11] Arslan M, Tüysüz N, Korkmaz S, Kurt H. Geochemistry and petrogenesis of the eastern Pontide volcanic rocks, Northeast Turkey. Chemie Der Erde Geochemistry 1997; 57:157–187.
[12] Özsayar T, Pelin S, Gedikoğlu A. Doğu Pontidlerde Kretase. KTÜ Yer Bilimleri Dergisi 1981; 1:65–114.
[13] Boztuǧ D, Erçin AI, Kuruçelik MK, Göç D, Kömür I, Iskenderoǧlu A. Geochemical characteristics of the composite Kaçkar batholith generated in a Neo-Tethyan convergence system, Eastern Pontides, Turkey. Journal of Asian Earth Sciences 2006; 27:286–302.
[14] Kaygusuz A, Siebel W, Şen C, Satir M. Petrochemistry and petrology of I-type granitoids in an arc setting: The composite Torul pluton, Eastern Pontides, NE Turkey. International Journal of Earth Sciences 2008; 97:739–764.
[15] Karslı O, Dokuz A, Uysal I, Aydin F, Chen B, Kandemir R, Wijbrans J. Relative contributions of crust and mantle to generation of Campanian high-K calc-alkaline I-type granitoids in a subduction setting, with special reference to the Harşit Pluton, Eastern Turkey. Contributions to Mineralogy and Petrology 2010; 160:467–487.
[16] Bektas O, Sen C, Atici Y, Köprübasi, Koprubasi N. Migration of the Upper Cretaceous subduction-related volcanism towards the back-arc basin of the eastern Pontide magmatic arc (NE Turkey). Geological Journal 1999; 34:95–106.
[17] Sipahi F. Zigana Dağı (Torul–Gümüşhane) Volkanitlerindeki Hidrotermal Ayrışmaların Mineraloji ve Jeokimyası. Karadeniz Teknik Üniversitesi, Trabzon, Türkiye, 2005.
[18] Eyüboǧlu Y. Late Cretaceous high-K volcanism in the eastern Pontide orogenic belt: Implications for the geodynamic evolution of NE Turkey. International Geology Review 2010; 52:142–186.
[19] Aydınçakır E, Kaygusuz A. Geç Kretase Yaşlı Dağbaşı (Araklı, Trabzon) Volkanitlerinin Petrografik ve Jeokimyasal Özellikleri, KD Türkiye. Gümüşhane Üniversitesi, Fen Bilimleri Enstitüsü Dergisi 2012; 2:123–142.
[20] Özdamar Ş. Geochemistry and geochronology of late Mesozoic volcanic rocks in the northern part of the Eastern Pontide Orogenic Belt (NE Turkey): Implications for the closure of the Neo-Tethys Ocean. Lithos 2016; 248–252:240–256.
[21] Yücel C, Arslan M, Temizel İ, Abdioğlu Yazar E, Ruffet G. Evolution of K-rich magmas derived from a net veined lithospheric mantle in an ongoing extensional setting: Geochronology and geochemistry of Eocene and Miocene volcanic rocks from Eastern Pontides (Turkey). Gondwana Research 2017; 45:65–86.
[22] Aydin F, Dokuz A, Kandemir R, Karsli O. Temporal , geochemical and geodynamic evolution of the Late Cretaceous subduction zone volcanism in the eastern Sakarya Zone , NE Turkey : implications for mantle-crust interaction in an arc setting 2020.
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Published
2021-12-31
How to Cite
Vural, A., & Kaygusuz, A. (2021). Petrographic and geochemical characteristics of Late Cretaceous volcanic rocks in the vicinity of Avliyana (Gümüşhane, NE Turkey). Journal of Engineering Research and Applied Science, 10(2), 1796-1810. Retrieved from http://www.journaleras.com/index.php/jeras/article/view/257
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