Zircon typology in granitoid rocks of the Ditró massif, Transylvania, Romania
The complex magmatic body of the Ditro Massif (Transylvania, Romania) was formed between the Middle Triassic and Lower Cretaceous times. Granitoid rocks can be found in a large area in the NE part of the massif. They were formed either by differentiation of an upper mantle ultramafic intrusion or by...
Elmentve itt :
| Szerzők: | |
|---|---|
| Dokumentumtípus: | Cikk |
| Megjelent: |
University of Szeged, Department of Mineralogy, Geochemistry and Petrology
Szeged
1999
|
| Sorozat: | Acta mineralogica-petrographica
40 |
| Kulcsszavak: | Kőzettan - Erdély, Ásványtan, Földtan |
| Tárgyszavak: | |
| Online Access: | http://acta.bibl.u-szeged.hu/24877 |