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...

Teljes leírás

Elmentve itt :
Bibliográfiai részletek
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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