Geochronology and geochemistry of the Miocene volcanics from the Kütahya area: Constraints for post-collisional magmatism in western Anatolia, Turkey

Özkul C., TEMİZEL İ., Özburan M., ARSLAN M., KİBİCİ Y.

Journal of African Earth Sciences, cilt.195, 2022 (SCI-Expanded) identifier

  • Yayın Türü: Makale / Tam Makale
  • Cilt numarası: 195
  • Basım Tarihi: 2022
  • Doi Numarası: 10.1016/j.jafrearsci.2022.104679
  • Dergi Adı: Journal of African Earth Sciences
  • Derginin Tarandığı İndeksler: Science Citation Index Expanded (SCI-EXPANDED), Scopus, Academic Search Premier, Aquatic Science & Fisheries Abstracts (ASFA), CAB Abstracts, Geobase, INSPEC
  • Anahtar Kelimeler: Geochronology, Isotope geochemistry, Kütahya, Miocene volcanics, Turkey, western Anatolia
  • Bilecik Şeyh Edebali Üniversitesi Adresli: Evet

Özet

© 2022 Elsevier LtdThe first geochronological and geochemical data are presented for the Kütahya area volcanics in western Turkey to study mantle sources and magmatic processes. Petrographically, the studied volcanics are composed primarily of olivine augite basalt and augite basalt, with minor basaltic andesites/trachyandesites, and show porphyric, hyalo-microlithic porphyric and rarely glomeroporphyric textures. The rock samples contain plagioclase as phenocrysts and microlites, olivine, augite and biotite as phenocrysts, sanidine, opaques, and volcanic glass. Whole-rock K–Ar dating of the studied volcanics yielded cooling ages between 20.1 ± 0.7 and 17 ± 0.5 Ma (Early Miocene). The volcanics indicate magma evolution from shoshonitic to medium-high-K character. High contents of LILEs and LREEs, and low amounts of Nb, Ta, Zr and Ti indicate that fractional crystallization and assimilation processes had a role in the evolution of these volcanics. The studied volcanics also have moderate to high 87Sr/86Sr (0.70719–0.70971), negative εNd values (−6.27 to −4.63), and high 206Pb/204Pb (18.93–19.05), 207Pb/204Pb (15.69–15.76) and 208Pb/204Pb (38.99–39.32) ratios. Integrated trace element geochemical and Sr-Nd-Pb-O isotopic data suggest that the Kütahya area volcanics evolved via AFC processes from parental magma(s) that originated from a subcontinental veined lithospheric mantle source metasomatized by subduction-related fluids and melts.