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
12th International Symposium on Water-Rock Interaction (WRI-12), Kunming, Çin, 31 Temmuz - 05 Ağustos 2007, ss.167-170, (Tam Metin Bildiri)
- Yayın Türü: Bildiri / Tam Metin Bildiri
- Cilt numarası:
- Basıldığı Şehir: Kunming
- Basıldığı Ülke: Çin
- Sayfa Sayıları: ss.167-170
- Süleyman Demirel Üniversitesi Adresli: Evet
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).