A new genetical ore formation model as a transition from Kuroko-type massive sulfide deposits to copper porphyries in the East Pontic metallotect, NE Turkey

Zerener M., Ozgur N., Elitok O.

12th International Symposium on Water-Rock Interaction (WRI-12), Kunming, Çin, 31 Temmuz - 05 Ağustos 2007, ss.167-170 identifier identifier

  • Cilt numarası:
  • Basıldığı Şehir: Kunming
  • Basıldığı Ülke: Çin
  • Sayfa Sayıları: ss.167-170

Özet

The Murgul deposit in the East Pontic metallotect is assigned to a subvolcanic formation connected with an Upper Cretaceous island arc volcanism developed temporally under subacrial conditions whereas the deposits at Madenkoy and Lahanos in the western part are genetically associated with a submarine hydrothermal activity in this volcanic sequence. There is a Cu-Mo belt in the northern part of the Anatolian micro plate. The Murgul deposit can be interpreted as a transition from Kuroko-type massive sulfide deposits to copper porphyries and might be considered as a new genetical model (Murgul type).