Chrome spinel geochemistry of ultramafic rocks from the Elekdag metaophiolite (Northern Turkey): Implications for greenschist to mid-amphibolite facies metamorphism

Gunay K., Donmez C., UYSAL İ., Yildirim N., Sahin M. B., YILDIRIM E., ...Daha Fazla

NEUES JAHRBUCH FUR MINERALOGIE-ABHANDLUNGEN, cilt.193, sa.3, ss.215-230, 2016 (SCI-Expanded) identifier identifier

  • Yayın Türü: Makale / Tam Makale
  • Cilt numarası: 193 Sayı: 3
  • Basım Tarihi: 2016
  • Doi Numarası: 10.1127/njma/2016/0303
  • Dergi Adı: NEUES JAHRBUCH FUR MINERALOGIE-ABHANDLUNGEN
  • Derginin Tarandığı İndeksler: Science Citation Index Expanded (SCI-EXPANDED), Scopus
  • Sayfa Sayıları: ss.215-230
  • Karadeniz Teknik Üniversitesi Adresli: Evet

Özet

The Elekdag metaophiolite is located in the central part of the Pontides orogenic belt in northern Anatolia, Turkey. This metaophiolite contains blueschist units, lawsonite eclogites and completely serpentinized ultramafic rocks, and is characterized by high pressure - low temperature metamorphism. The collision and accretion processes that prevailed in the central Pontides during the Albian-Santonian interval play an important role in metamorphism of the Elekdag metaophiolite and associated units.