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
-
Anahtar Kelimeler:
Late Cretaceous, Subduction, Volcanism, Mantle-crust interaction, Sakarya Zone, Eastern Pontides, NE Turkey, PONTIDE OROGENIC BELT, I-TYPE GRANITOIDS, CONTINENTAL-CRUST, ISOTOPIC CHARACTERISTICS, NEOTETHYAN CONVERGENCE, GUMUSHANE AREA, ARTVIN AREA, ROCKS, MAGMATISM, PETROGENESIS
-
Karadeniz Teknik 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.