Chromite and PGE geochemistry of the Elekdag Ophiolite (Kastamonu, Northern Turkey): Implications for deep magmatic processes in a supra-subduction zone setting

Donmez, Cahit; Keskin, Serdar; Gunay, Kurtulus; Colakoglu, Aydin; Ciftci, Yahya; UYSAL, İBRAHİM; Turkel, Aytekin; Yildinm, Nail

doi:10.1016/j.oregeorev.2013.09.019

Chromite and PGE geochemistry of the Elekdag Ophiolite (Kastamonu, Northern Turkey): Implications for deep magmatic processes in a supra-subduction zone setting

Atıf İçin Kopyala

Donmez C., Keskin S., Gunay K., Colakoglu A. O., Ciftci Y., UYSAL İ., ...Daha Fazla

ORE GEOLOGY REVIEWS, cilt.57, ss.216-228, 2014 (SCI-Expanded)

Yayın Türü: Makale / Tam Makale
Cilt numarası: 57
Basım Tarihi: 2014
Doi Numarası: 10.1016/j.oregeorev.2013.09.019
Dergi Adı: ORE GEOLOGY REVIEWS
Derginin Tarandığı İndeksler: Science Citation Index Expanded (SCI-EXPANDED), Scopus
Sayfa Sayıları: ss.216-228
Anahtar Kelimeler: Chromite, Deep magma processes, Platinum group elements (PGE), Elekdag ophiolite, Kastamonu, Northern Turkey, PLATINUM-GROUP ELEMENTS, MELT-ROCK INTERACTION, THETFORD MINES OPHIOLITE, MID-ATLANTIC RIDGE, PODIFORM CHROMITITES, CENTRAL PONTIDES, GROUP MINERALS, SW TURKEY, OMAN OPHIOLITE, CAPE-VOGEL
Karadeniz Teknik Üniversitesi Adresli: Evet

Özet

The geochemistry of chromium spinel and platinum group elements (PGE) provides significant information about conditions in the mantle during the emplacement and genesis of ophiolitic complexes. The Elekdag ophiolite is a greenschist to amphibolite facies ophiolite that was emplaced onto the Sakarya Zone, in the central part of the Pontides of northern Turkey. NW-SE trending Elekdag ophiolite hosts small scale chromitite occurrences in serpentinized harzburgite and dunite, and have maximum resource of several thousands t Cr2O3.