Petrogenesis of Maktali fractionated calc-alkaline younger granitoids, Central Eastern Desert, Egypt
Author:
Publisher
Springer Science and Business Media LLC
Subject
General Earth and Planetary Sciences,General Environmental Science
Link
http://link.springer.com/content/pdf/10.1007/s12517-019-4559-x.pdf
Reference79 articles.
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2. Abdelsalam MG, Stern RJ (1996) Sutures and shear zones in the Arabian Nubian Shield. J Afr Earth Sci 23:289–310. https://doi.org/10.1016/S0899-5362(97)00003-1
3. Abdelsalam MG, Liégeois J-P, Stern RJ (2002) The Saharan metacraton. J Afr Earth Sci 34:119–136. https://doi.org/10.1016/S0899-5362(02)00013-1
4. Agrawal S (1995) Discrimination between late-orogenic, post-orogenic, and anorogenic granites by major element compositions. J Geol 103:529–537. https://doi.org/10.1086/629774
5. Ali KA, Moghazi AM, Maurice AE, Omar SA, Wang Q, Wilde SA, Moussa EM, Manton WI, Stern RJ (2012) Composition, age, and origin of the ~ 620 Ma Humr Akarim and Humrat Mukbid A-type granites: no evidence for pre-Neoproterozoic basement in the Eastern Desert, Egypt. Int J Earth Sci 101(7):1705–1722. https://doi.org/10.1007/s00531-012-0759-2
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