Mohamed, F.H. and Hassan, M.A. (1996) Geochemical Evolution of Arc-Related Mafic Magmatism at Hmm Naggat District, Eastern Desert of Egypt. Journal of African Earth Sciences, 22, 29-42.
http://dx.doi.org/10.1016/0899-5362(96)00018-8

has been cited by the following article:

• TITLE: Petrology and Geochemical Characteristic of the Younger Gabbros of Wadi Shianite Area, Southeastern Desert, Egypt

  AUTHORS: Magdy S. Basta

  KEYWORDS: Pyroxene Hornblende Gabbronorite, Hornblende Gabbro and Anorthosite

  JOURNAL NAME: Open Journal of Geology, Vol.5 No.8, August 28, 2015

  ABSTRACT: The present work is a petrological study of the gabbroic rocks of wadi Shianite Southeastern Desert of Egypt. Chemical analyses for major and trace elements showed that there are 3 main gabbro types. These are: 1)pyroxene hornblende gabbronorite;2) hornblende gabbro;and 3) anorthosite.The opaque minerals study of the gabbroic rocks showed that they composed mainly of ilmenite, magnetite and sulphides. The present gabbroic rocks work are related to calc-alkaline magma type, similar to the younger gabbros in other areas in the Eastern Desert.