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...
Elmentve itt :
| 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 |
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