Geochemistry and mineral chemistry of Pan-African amphibolites of South Sinai, Egypt

Mohamed El-Tokhi, Bahaa Eldin Amin, Sulaiman Alabeed, Abdulla Musallam

Research output: Contribution to journalArticlepeer-review

3 Citations (Scopus)


In the Wadi Feiran area, amphibolites occur as inclusions, bands, linear bodies of variable thickness and irregular lenses in para-geneisses. Chemical evidence indicates that these amphibolites display an igneous origin and were derived from magma essentially of tholelitic rather than alkaline composition; transitional in character between continental and island-arc. The chemistry of amphiboles, related to pressure and temperature conditions of metamorphism, showed that they were formed under low pressure and high temperature conditions.

Original languageEnglish
Pages (from-to)246-254
Number of pages9
JournalChinese Journal of Geochemistry
Issue number3
Publication statusPublished - Sept 2010


  • Pan-African amphibolite
  • Sinai, Egypt
  • geochemistry
  • mineral chemistry

ASJC Scopus subject areas

  • Geochemistry and Petrology


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