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, ss.215-230, 2016 (SCI İndekslerine Giren Dergi) identifier identifier

  • Cilt numarası: 193 Konu: 3
  • Basım Tarihi: 2016
  • Doi Numarası: 10.1127/njma/2016/0303
  • Dergi Adı: NEUES JAHRBUCH FUR MINERALOGIE-ABHANDLUNGEN
  • Sayfa Sayıları: ss.215-230

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.