The ophiolite melange of Wadi Dunquash and Arayis, Eastern desert of Egypt petrogenesis and tectonic evolution /

Wadi Dunqash and Wadi Arayis in the central and southern Eastern Desert of Egypt are characterized by the presence of metamorphosed dismembered ophiolite sequence. This sequence consists of harzburgiteserpentinite, pyroxenite-chlorite schist; normal and sheared metagabbros; metabasalt and meta-andes...

Teljes leírás

Elmentve itt :
Bibliográfiai részletek
Szerzők: Abdel-Karim Abdel-Aal Mohamed
El-Mahallawy M. M.
Finger F.
Dokumentumtípus: Cikk
Megjelent: University of Szeged, Department of Mineralogy, Geochemistry and Petrology Szeged 1996
Sorozat:Acta mineralogica-petrographica 37
Kulcsszavak:Kőzettan, Ásványtan, Földtan
Tárgyszavak:
Online Access:http://acta.bibl.u-szeged.hu/24838

Hasonló tételek