Behaviour of major elements in the granitic rocks of Kadabora pluton, Eastern Desert, Egypt

The petrochemical features of the granitic rocks of Kadabora pluton, Eastern Desert, Egypt are presented. Results of twenty new chemical analyses are advanced and processed following several petrochemical parameters. The average chemical composition of Kadabora granitic rocks is in harmony with that...

Teljes leírás

Elmentve itt :
Bibliográfiai részletek
Szerzők: Kabesh Mahmoud Lofty
Hilmy Mohamed Ezzeldin
Salem Abdel-Karim Ahmed
Dokumentumtípus: Cikk
Megjelent: University of Szeged, Department of Mineralogy, Geochemistry and Petrology Szeged 1980
Sorozat:Acta mineralogica-petrographica 24 No. 2
Kulcsszavak:Kőzettan, Ásványtan, Földtan
Tárgyszavak:
Online Access:http://acta.bibl.u-szeged.hu/24657
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245 1 0 |a Behaviour of major elements in the granitic rocks of Kadabora pluton, Eastern Desert, Egypt  |h [elektronikus dokumentum] /  |c  Kabesh Mahmoud Lofty 
260 |a University of Szeged, Department of Mineralogy, Geochemistry and Petrology  |b Szeged  |c 1980 
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490 0 |a Acta mineralogica-petrographica  |v 24 No. 2 
520 3 |a The petrochemical features of the granitic rocks of Kadabora pluton, Eastern Desert, Egypt are presented. Results of twenty new chemical analyses are advanced and processed following several petrochemical parameters. The average chemical composition of Kadabora granitic rocks is in harmony with that of low-calcium granite of TUREKIAN and WEDEPOHL [1961]. The granitic rocks possess in general rather pronounced potassic characters with few sodic affinities. Chemical classification of the granitic rocks is attempted. Magmatic origin is suggested for the examined granitic rocks and is based on experimentally studied systems. 
650 4 |a Természettudományok 
650 4 |a Föld- és kapcsolódó környezettudományok 
695 |a Kőzettan, Ásványtan, Földtan 
700 0 1 |a Hilmy Mohamed Ezzeldin  |e aut 
700 0 1 |a Salem Abdel-Karim Ahmed  |e aut 
856 4 0 |u http://acta.bibl.u-szeged.hu/24657/1/mineralogica_024_fasc_002_245-256.pdf  |z Dokumentum-elérés