Harris, N.B.W., Pearce, J.A. and Tendle, A.G. (1986) Geochemical Characteristics of Collision-Zone Magmatism. In: Coward, M.P. and Ries, A.C., Eds., Collision Tectonics, Spec. Publ. Geol. Soc. 19, London, 67-81.
https://doi.org/10.1144/GSL.SP.1986.019.01.04

has been cited by the following article:

• TITLE: Characterization of a Post Orogenic A-Type Granite, Gabal El Atawi, Central Eastern Desert, Egypt: Geochemical and Radioactive Perspectives

  AUTHORS: Khairiya M. Fawzy

  KEYWORDS: Radioactivity, Geochemistry, Post-Orogenic, A-Type Granite, Gabal El Atawi, Central Eastern Desert, Egypt

  JOURNAL NAME: Open Journal of Geology, Vol.7 No.1, January 25, 2017

  ABSTRACT: The alkali feldspar granite of Gabal El Atawi is post orogenic granite originated from subalkaline magma in extensional suite. It is developed within plate tectonic setting and has A2-type character which generated from apparent crustal source. The petrographic, geochemical and radioactive characteristics of El Atawi granite meet and fulfill the requirements of being fertile granite and it can be considered as promising uraniferous granite. Fluid inclusion studies of the altered granite elucidated two different solutions acting on the host granitic pluton. The first is NaCl-CaCl low temperature fluid with a wide range of salinity. The second is high temperature and salinity Fe-Mg-Na chloride solution. Different fractures in the granite acted as good channels for the hydrothermal fluids that leached uranium from its bearing minerals disseminated all over the host granite and redeposited it in the alteration zones.