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

AYDIN, FARUK; OĞUZ SAKA, SİMGE; ŞEN, CÜNEYT; DOKUZ, ABDURRAHMAN; Aiglsperger, Thomas; UYSAL, İBRAHİM; Kandemir, RAİF; Karsli, ORHAN; San, Bilal; Baser, Rasim

doi:10.1016/j.jseaes.2019.104217

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

Atıf İçin Kopyala

AYDIN F., OĞUZ SAKA S., ŞEN C., DOKUZ A., Aiglsperger T., UYSAL İ., ...Daha Fazla

JOURNAL OF ASIAN EARTH SCIENCES, cilt.192, 2020 (SCI-Expanded)

Yayın Türü: Makale / Tam Makale
Cilt numarası: 192
Basım Tarihi: 2020
Doi Numarası: 10.1016/j.jseaes.2019.104217
Dergi Adı: JOURNAL OF ASIAN EARTH SCIENCES
Derginin Tarandığı İndeksler: Science Citation Index Expanded (SCI-EXPANDED), Scopus, Academic Search Premier, Artic & Antarctic Regions, Geobase, INSPEC
Recep Tayyip Erdoğan Üniversitesi Adresli: Evet

Özet

The Late Cretaceous Artvin volcanic rocks (LCAVs) from the eastern Sakarya zone (ESZ) of NE Turkey are composed of mafic/basaltic (S1-catak and S2-caglayan) and felsic/acidic (S1-Kizilkaya and S2-Tirebolu) rock types that occurred in two successive stages: (i) first stage (S1: Turonian-Early Santonian) and (ii) second stage (S2: Late Santonian-Campanian). Clinopyroxene thermobarometric results point that the S2-caglayan basaltic rocks have crystallised at higher temperatures and under deeper crustal conditions than those of the S1-catak basaltic rocks.