Abstract
Poly-deformed late-Proterozoic metamorphic domains covering Um Ashira area at the western segment of Wadi Allaqi shear zone, South Eastern Desert of Egypt, show evidences of inverted Barrovian metamorphism. They exhibit four metamorphic zonal patterns, arranging progressively from chlorite, biotite, garnet, to sillimanite zones. The higher grade metamorphic domains appear at higher structural levels with general dipping toward the North East. Four deformational phases (D1–D4), associating with major planar structures (S1–S4), and four mesoscopic and microscopic folds are recognized. The pervasive fabric, growth of metamorphic minerals and peak metamorphism were linked to D2 deformation phase. Structural, petrographic, microchemical, and thermobarometric data along South-North profile show possibility of inverted Barrovian metamorphic pattern with an increase in the metamorphic grade toward the North. The established structural sequence and tectonic modeling suggest that the apparent inversion coexists due to the main F2 folding phase.
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ACKNOWLEDGMENTS
The authors highly acknowledge the Geology Department, Faculty of Science, Aswan University (Egypt), for allowing the field facilities and petrographic studies.
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Radwan, A., El Fakharani, A., Abbas, H. et al. Inverted Barrovian Metamorphic Zones in the Poly-Deformed Domains of the Western Wadi Allaqi Shear Zone (South Eastern Desert, Egypt): Geochemical and Structural Constraints. Geotecton. 55, 94–111 (2021). https://doi.org/10.1134/S0016852121010118
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DOI: https://doi.org/10.1134/S0016852121010118