Zircon in granitoids from Sinai, Egypt and its genetic significance

Heikal Mohamed A. and Salem Abdel-Karim Ahmed and El-Sheshtawi Youssef A.: Zircon in granitoids from Sinai, Egypt and its genetic significance. In: Acta mineralogica-petrographica, (27). pp. 117-130. (1985)

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Abstract

The granitic plutonism in the area around Wadi El-Sheikh, southwestern Sinai, Egypt is mainly represented by the Older and Younger Granitoid Rocks. The younger granitic rocks comprise in turn, two granitic phases, distinguished on field basis. Morphological characters of zircon concentrates from the examined rocks have been statistically studied. Zircon populations in the Older Granitoids contain a wide variety of crystal shapes while in those of the younger granitic rocks, zircon crystals become prograssively more uniform in morphology. Distinction between zircons of the Older and Younger Granitoids is based mainly on their dimensional parameters. Similarity of the dimensional parameters of zirkons in the younger granitic phases renders their separation difficult. The significance of zircon as a guide to the pedogenesis of Wadi El-Sheikh granitoids is ascertained.

Item Type: Article
Journal or Publication Title: Acta mineralogica-petrographica
Date: 1985
Volume: 27
ISSN: 0365-8066
Page Range: pp. 117-130
Language: English
Publisher: University of Szeged, Department of Mineralogy, Geochemistry and Petrology
Place of Publication: Szeged
Related URLs: http://acta.bibl.u-szeged.hu/39405/
Uncontrolled Keywords: Kőzettan, Ásványtan, Földtan
Additional Information: Bibliogr.: p. 129-130. ; ill. ; összefoglalás angol nyelven
Subjects: 01. Natural sciences
01. Natural sciences > 01.05. Earth and related environmental sciences
Date Deposited: 2016. Oct. 17. 09:25
Last Modified: 2022. Jul. 26. 10:44
URI: http://acta.bibl.u-szeged.hu/id/eprint/24732

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