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

Özdamar Ş.

LITHOS, cilt.248, ss.240-256, 2016 (SCI-Expanded) identifier identifier

  • Yayın Türü: Makale / Tam Makale
  • Cilt numarası: 248
  • Basım Tarihi: 2016
  • Doi Numarası: 10.1016/j.lithos.2016.01.007
  • Dergi Adı: LITHOS
  • Derginin Tarandığı İndeksler: Science Citation Index Expanded (SCI-EXPANDED), Scopus
  • Sayfa Sayıları: ss.240-256
  • Anahtar Kelimeler: 40Ar/39Ar ages, Zircon U-P dating, Sr-Nd isotope composition, Eastem Pontide, Neo-Tethys, NE Turkey, GEODYNAMIC EVOLUTION, CONTINENTAL-CRUST, ISOTOPE GEOCHEMISTRY, GUMUSHANE AREA, MAGMA CHAMBER, SAKARYA ZONE, ARC MAGMAS, PETROGENESIS, SUBDUCTION, SR
  • İstanbul Teknik Üniversitesi Adresli: Evet

Özet

This paper presents Ar-46/Ar-39 and U-Pb age data, Sr-Nd isotopes, whole-rock and mineral compositions of Upper Cretaceous volcanic rocks from the Ordu area of the Eastern Pontide Orogenic Belt (EPOB) in northeastern Turkey. The volcanic rocks exhibit a wide compositional range: basalt, basaltic-andesites, andesites and a rhyodacite suite; they are characterized by subparallel light rare earth element (LREE)-enrichment, relatively flat heavy rare earth element (HREE) patterns with Eu anomalies and moderate fractionation [average (La/Yb)N = 8.55]. The geochemical results show that the volcanic rocks have calc-alkaline affinity consistent with arc volcanic rocks erupted in an active continental margin. Initial Sr-87/Sr-86 values vary between 0.70569 and 0.70606, while initial Nd-143/Nd-144 values lie between 0.51244 and 0.51249. Crustal contamination affected the mantle-originated primary magma, as indicated by increased Sr-87/Sr-86 and decreased Nd-143/Nd-144 ratios with increasing SiO2. New precise laser ablation inductively coupled plasma mass spectrometer (LA-ICP-MS) Pb-206-U-238 age analyses of zircon and Ar-40/Ar-39 age data of plagioclase from the volcanics enable a more precise reconstruction of the EBOP. The ages provide insight into the timing of arc formation in this region, constrain the volcanic activity between 86 My (Coniacian) and 75 My (Campanian) and constrain the timing of closure of the Neo-Tethys. (C) 2016 Elsevier B.V. All rights reserved.