Preliminary zircon fission track results in the Kőszeg Penninic unit, W. Hungary
Zircon fission track ages were determined in quartzphyllite samples of the Hungarian side of the Koszeg-Rechnitz Penninic series. The data scatter between 15.1 and 18.5 My, showing a slight areal variability which calls attention to different uplift rates in the unit. The results agree well with lit...
Elmentve itt :
| Szerzők: | |
|---|---|
| Dokumentumtípus: | Cikk |
| Megjelent: |
University of Szeged, Department of Mineralogy, Geochemistry and Petrology
Szeged
1991
|
| Sorozat: | Acta mineralogica-petrographica
32 |
| Kulcsszavak: | Kőzettan, Ásványtan, Földtan |
| Tárgyszavak: | |
| Online Access: | http://acta.bibl.u-szeged.hu/24791 |
| Tartalmi kivonat: | Zircon fission track ages were determined in quartzphyllite samples of the Hungarian side of the Koszeg-Rechnitz Penninic series. The data scatter between 15.1 and 18.5 My, showing a slight areal variability which calls attention to different uplift rates in the unit. The results agree well with literature data gathered from far-lying Penninic units, that means, that the uplift of the Penninic Biindnerschiefer series might have taken place in the same time interval throughout the whole Alps. |
|---|---|
| Terjedelem/Fizikai jellemzők: | 43-47 |
| ISSN: | 0365-8066 |