| dc.creator |
Ozgur, N. |
|
| dc.date |
2010-01-01T01:00:00Z |
|
| dc.date.accessioned |
2021-12-03T11:20:39Z |
|
| dc.date.available |
2021-12-03T11:20:39Z |
|
| dc.identifier |
40689870-6823-4891-8005-41f465af95bb |
|
| dc.identifier |
https://avesis.sdu.edu.tr/publication/details/40689870-6823-4891-8005-41f465af95bb/oai |
|
| dc.identifier.uri |
http://acikerisim.sdu.edu.tr/xmlui/handle/123456789/91119 |
|
| dc.description |
The Murgul deposit in the East Pontic metallotect is assigned to a subvolcanic formation related to an Upper Cretaceous island arc temporally developed under subaerial conditions, whereas the deposits at Madenkoy and Lahanos, in the western part, are genetically associated with a submarine hydrothermal activity. There is a Cu-Mo belt in the northern part of the Anatolian microplate. The Cu deposit of Murgul can be interpreted as a transition from Kuroko-type volcanogenic massive sulfides (VMS) to porphyry copper deposits and might be viewed as a new ore deposit model (Murgul type). |
|
| dc.language |
eng |
|
| dc.rights |
info:eu-repo/semantics/closedAccess |
|
| dc.title |
A new genetical copper deposit model from the East Pontic metallotect, NE Turkey: The Murgul type |
|
| dc.type |
info:eu-repo/semantics/conferenceObject |
|