lliase, E., Shahata, R., Kandil, K., Samaan, J. (2008). PETROGRAPHY AND MINERAL CHEMISTRY AT WADI BALLI AREA, CENTRAL EASTERN DESERT, EGYPT. test, 32(1), 68-76. doi: 10.21608/djs.2008.152958
Emile L. lliase; Raafat M.S. Shahata; Kandil M. Kandil; Joseph M. Samaan. "PETROGRAPHY AND MINERAL CHEMISTRY AT WADI BALLI AREA, CENTRAL EASTERN DESERT, EGYPT". test, 32, 1, 2008, 68-76. doi: 10.21608/djs.2008.152958
lliase, E., Shahata, R., Kandil, K., Samaan, J. (2008). 'PETROGRAPHY AND MINERAL CHEMISTRY AT WADI BALLI AREA, CENTRAL EASTERN DESERT, EGYPT', test, 32(1), pp. 68-76. doi: 10.21608/djs.2008.152958
lliase, E., Shahata, R., Kandil, K., Samaan, J. PETROGRAPHY AND MINERAL CHEMISTRY AT WADI BALLI AREA, CENTRAL EASTERN DESERT, EGYPT. test, 2008; 32(1): 68-76. doi: 10.21608/djs.2008.152958

PETROGRAPHY AND MINERAL CHEMISTRY AT WADI BALLI AREA, CENTRAL EASTERN DESERT, EGYPT

Delta Journal of Science
Article 6, Volume 32, Issue 1, June 2008, Pages 68-76    PDF (4.09 M)
Document Type: Research and Reference
DOI: 10.21608/djs.2008.152958
Authors
Emile L. lliase; Raafat M.S. Shahata; Kandil M. Kandil; Joseph M. Samaan
Nuclear Materials Authority, P. O. Box 530, Maadi, Cairo, Egypt
Abstract
The Gattar granites are composed mainly of quartz and feldspars as essential minerals and biotite hornblende, zircon, apatite and sphene as accessory minerals, some secondary minerals as epidote, chlorite and sericite are found. The Gattar granites originated from calc-alkaline magma and tectonically it is volcanic arc granites. The study includes some mineral as feldspars, biotite and, amphiboles from Wadi Balli under Environmental Scanning electron Microscopy (ESEM) attached by Energy Dispersive E-ray analyses (EDX) in nuclear Materials Authority (NMA), gave that the feldspars composed under temperature 850ºC and biotite in Wadi Balli originated from magmatic origin.
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