USTAÖMER, T. Et Al. 2014. 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). European Geoscience Union , (Viyana, Austria), 10091.

USTAÖMER, T., Ustaömer, P. A., Robertson, A. H., Gerdes, A., & Zulauf, G., (2014). 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) . European Geoscience Union (pp.10091). Viyana, Austria

USTAÖMER, Timur Et Al. "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)," European Geoscience Union, Viyana, Austria, 2014

USTAÖMER, Timur Et Al. "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)." European Geoscience Union , Viyana, Austria, pp.10091, 2014

USTAÖMER, T. Et Al. (2014) . "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)." European Geoscience Union , Viyana, Austria, p.10091.

@conferencepaper{conferencepaper, author={Timur USTAÖMER Et Al. }, title={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)}, congress name={European Geoscience Union}, city={Viyana}, country={Austria}, year={2014}, pages={10091} }