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
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 subaerial conditions whereas the deposits at Madenk(o)y 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).
M.Zerener N.(O)zgür (O).Elitok
Süleyman (U)niversitesi, Research and Application Centre for Geothermal Energy, Groundwater and Mineral Resources, Isparta, Turkey
国际会议
第十二届水-岩相互作用国际研讨会(P0roceedings of the 12th International Symposium on Water-Rock Interaction)
昆明
英文
167-170
2007-07-31（万方平台首次上网日期，不代表论文的发表时间）