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)

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

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

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