| dc.creator |
Isik, Kayhan |
|
| dc.creator |
CENGİZ, Oya |
|
| dc.creator |
Kuscu, Mustafa |
|
| dc.creator |
Gul, E. Kubra |
|
| dc.date |
2018-06-30T21:00:00Z |
|
| dc.date.accessioned |
2020-10-06T12:02:27Z |
|
| dc.date.available |
2020-10-06T12:02:27Z |
|
| dc.identifier |
f56d6dc6-a1e7-4b57-9bb4-682fde145dd3 |
|
| dc.identifier |
10.1016/j.jafrearsci.2018.03.013 |
|
| dc.identifier |
https://avesis.sdu.edu.tr/publication/details/f56d6dc6-a1e7-4b57-9bb4-682fde145dd3/oai |
|
| dc.identifier.uri |
http://acikerisim.sdu.edu.tr/xmlui/handle/123456789/76295 |
|
| dc.description |
Rutile occur in important amounts within Quaternary detrital sediments, and quartz veins which cut down the Paleozoic aged Esme formation in the Menderes Massif on the Neoproterozoic Pan-Afrikan Belt in the west of Turkey. As a result of erosion, transport and accumulation of rutile-bearing quartz veins in the mica schists of the Esme formation outcropped between Esme (Usak) and Kula (Manisa), the placer rutile occurrences occur in terraces, fluvial-alluvial and eluvial deposits. This study investigates the element content of rutile, oxygen isotope ratios of rutile and quartz, and formation temperature of rutile related to titanium source rock. |
|
| dc.language |
eng |
|
| dc.rights |
info:eu-repo/semantics/closedAccess |
|
| dc.title |
The origin and geochemical characteristics of rutile in eluvial and fluvial-alluvial placers and quartz veins of the Menderes Massif from the Neoproterozoic Pan-African Belt, Western Turkey |
|
| dc.type |
info:eu-repo/semantics/article |
|