Origin and tectonic history of some metamorphic rocks from Southern Sinai, Egypt
The Baba schists and gneisses, in the extremely northwestern part of the metamorphic belt of Sinai, have been discussed in terms of the mode of occurrence, evolution of mineral chemistry, major, trace and rare earth elements (REE) and age dating. They exhibit a trondhjemitic composition and comprise...
Elmentve itt :
| Szerzők: |
Abdel-Karim Abdel-Aal Mohamed Puskás Zuard Jánosi Melinda |
|---|---|
| Dokumentumtípus: | Cikk |
| Megjelent: |
Department of Mineralogy, Geochemistry and Petrology, University of Szeged
Szeged
2002
|
| Sorozat: | Acta mineralogica-petrographica
43 |
| Kulcsszavak: | Földtan, Kőzettan, Ásványtan |
| Tárgyszavak: | |
| Online Access: | http://acta.bibl.u-szeged.hu/25095 |
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