Geochemical studies of some granites from the South Western Desert, Egypt

The present work is the first detailed petrochemical and geochemical studies done on some 18 granitic rocks collected from the south Western Desert of Egypt. The petrochemical work includes complete chemical analyses of these rocks beside calculation of the CIPW norms,- NIGGLI values, D. I. , F. I....

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Elmentve itt :
Bibliográfiai részletek
Szerzők: El Sokkary A. A.
El Ramly M. F.
Salloum G. M.
Aly Monir M.
Dokumentumtípus: Cikk
Megjelent: University of Szeged, Department of Mineralogy, Geochemistry and Petrology Szeged 1978
Sorozat:Acta mineralogica-petrographica 23 No. 2
Kulcsszavak:Kőzettan, Ásványtan, Földtan, Geokémia
Tárgyszavak:
Online Access:http://acta.bibl.u-szeged.hu/24631
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040 |a SZTE Egyetemi Kiadványok Repozitórium  |b hun 
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100 2 |a El Sokkary A. A. 
245 1 0 |a Geochemical studies of some granites from the South Western Desert, Egypt  |h [elektronikus dokumentum] /  |c  El Sokkary A. A. 
260 |a University of Szeged, Department of Mineralogy, Geochemistry and Petrology  |b Szeged  |c 1978 
300 |a 223-237 
490 0 |a Acta mineralogica-petrographica  |v 23 No. 2 
520 3 |a The present work is the first detailed petrochemical and geochemical studies done on some 18 granitic rocks collected from the south Western Desert of Egypt. The petrochemical work includes complete chemical analyses of these rocks beside calculation of the CIPW norms,- NIGGLI values, D. I. , F. I. and M . I. Thirteen trace elements are quantitatively determined, these are: Ba, Rb, Sr, Y, Zr, Nb, La, Ce, Nd, Cr, Ni, Zn and Cu. These chemical studies established the presence of five rock types: grey granite, Aswan-type granite, normal pink-red granite, strongly fractionated pink-red granite and syenite.'It is concluded that the basement rocks of Egypt developed in the Eastern Desert and Sinai peninsula are extended across the Nile, mostly subsurface, in the southern parts of the Western Desert. To the first time, Aswan coarse granites are proved to occur in the south Western Desert. This makes them of much wider aereal distribution than previously known. On account of their peculiar chemical composition, Aswan plutonites can be grouped in a separate plutonic cycle. 
650 4 |a Természettudományok 
650 4 |a Föld- és kapcsolódó környezettudományok 
695 |a Kőzettan, Ásványtan, Földtan, Geokémia 
700 0 2 |a El Ramly M. F.  |e aut 
700 0 2 |a Salloum G. M.  |e aut 
700 0 2 |a Aly Monir M.  |e aut 
856 4 0 |u http://acta.bibl.u-szeged.hu/24631/1/mineralogica_023_fasc_002_223-237.pdf  |z Dokumentum-elérés