GEOLOGY AND PETROGRAPHY OF MUBARAK AREA, CENTRAL EASTERN DESERT, EGYPT

Authors

  • Mohamed Abdelhadi BADAWI Mansoura University
  • Farid M. Ali MAKROUM Mansoura University
  • Ahmed SHALABY Mansoura University
  • Norbert NÉMETH University of Miskolc

DOI:

https://doi.org/10.33030/geosciences.2021.14.005

Keywords:

granite, Pan-African Orogeny, intrusive, Island Arc Association

Abstract

The Mubarak region is covered by two major rock units: the Island Arc Associa- tion and granitoids. This Island Arc Association is represented by metaandesite, hornblende- actinolite schist, and amphibolite, which were metamorphosed up to amphibolite facies. Granitoids are classified based on the petrographic mineral composition into two phases: the syn- to late-orogenic phase and the post-orogenic phase. According to field observations and petrographic analyses, these granitoids are magmatic rocks with isotropic texture, as opposed to the Island Arc Association, which is strongly foliated, indicating that a NW shortening occurred prior to the emplacement of the weakly metamorphosed granodiorite and the non- metamorphic post-orogenic intrusives.

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Published

2022-05-11

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Articles