| dc.creator |
Ozgur, N. |
|
| dc.creator |
Zerener, M. |
|
| dc.creator |
Elitok, O. |
|
| dc.date |
2006-12-31T22:00:00Z |
|
| dc.date.accessioned |
2020-10-06T10:50:45Z |
|
| dc.date.available |
2020-10-06T10:50:45Z |
|
| dc.identifier |
a10866ca-41f5-404e-b6df-875f365e2e7e |
|
| dc.identifier |
https://avesis.sdu.edu.tr/publication/details/a10866ca-41f5-404e-b6df-875f365e2e7e/oai |
|
| dc.identifier.uri |
http://acikerisim.sdu.edu.tr/xmlui/handle/123456789/67922 |
|
| dc.description |
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). |
|
| dc.language |
eng |
|
| dc.rights |
info:eu-repo/semantics/closedAccess |
|
| dc.title |
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 |
|
| dc.type |
info:eu-repo/semantics/conferenceObject |
|