2021
DOI: 10.33030/geosciences.2021.14.005
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Geology and Petrography of Mubarak Area, Central Eastern Desert, Egypt

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 isotro… Show more

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“…According to the geological setting (Fig. 1 ), El Rukham- Mueilha district is occupied by various lithologies, including suprastructural Neoproterozoic Pan-African nappe assemblage (dismembered masses of ophiolitic mélange and island arc association) and syn to post-orogenic intrusive rocks which represents the main geological units within the Barramiya-Mubarak sector 88 . These lithologies are heavily altered by the magmatic fluids in the name of hematization (Fig.…”
Section: Field Verification and Petrographic Investigationsmentioning
confidence: 99%
“…According to the geological setting (Fig. 1 ), El Rukham- Mueilha district is occupied by various lithologies, including suprastructural Neoproterozoic Pan-African nappe assemblage (dismembered masses of ophiolitic mélange and island arc association) and syn to post-orogenic intrusive rocks which represents the main geological units within the Barramiya-Mubarak sector 88 . These lithologies are heavily altered by the magmatic fluids in the name of hematization (Fig.…”
Section: Field Verification and Petrographic Investigationsmentioning
confidence: 99%