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 T., Ustaömer P. A., Robertson A. H., Gerdes A., Zulauf G.

European Geoscience Union, Viyana, Austria, 27 April - 02 May 2014, vol.16, pp.10091

  • Publication Type: Conference Paper / Summary Text
  • Volume: 16
  • City: Viyana
  • Country: Austria
  • Page Numbers: pp.10091
  • Istanbul University Affiliated: Yes