Triassic arc-derived detritus in the Triassic Karakaya accretionary complex was not derived from either the S Eurasian margin (Istanbul terrane) or the N Gondwana margin (Taurides)

USTAÖMER P. A., Robertson A. H., Gerdes A., Zulauf G.

EGU-2014 (European Union of GeoSciences) Meeting, 01 Nisan 2014

  • Yayın Türü: Bildiri / Tam Metin Bildiri
  • Yıldız Teknik Üniversitesi Adresli: Evet