Arid
DOI10.1134/S0016852121010118
Inverted Barrovian Metamorphic Zones in the Poly-Deformed Domains of the Western Wadi Allaqi Shear Zone (South Eastern Desert, Egypt): Geochemical and Structural Constraints
Radwan, A.; El Fakharani, A.; Abbas, H.; Younis, M. H.; Emam, A.; Fawzy, Sh
通讯作者Younis, MH (corresponding author), Aswan Univ, Fac Sci, Dept Geol, Aswan 81528, Egypt.
来源期刊GEOTECTONICS
ISSN0016-8521
EISSN1556-1976
出版年2021
卷号55期号:1页码:94-111
英文摘要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 (D-1-D-4), associating with major planar structures (S-1-S-4), and four mesoscopic and microscopic folds are recognized. The pervasive fabric, growth of metamorphic minerals and peak metamorphism were linked to D-2 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 F-2 folding phase.
英文关键词Inverted Barrovian metamorphism Wadi Allaqi shear zone tectonic model thermobarometry South Eastern Desert Egypt
类型Article
语种英语
收录类别SCI-E
WOS记录号WOS:000644867300006
WOS关键词TEMPERATURE-TIME PATHS ; EXPERIMENTAL CALIBRATION ; PRESSURE ; HORNBLENDE ; ISOGRADS ; SEQUENCE ; COMPLEX ; GARNET ; GREENSCHIST ; SILLIMANITE
WOS类目Geochemistry & Geophysics
WOS研究方向Geochemistry & Geophysics
资源类型期刊论文
条目标识符http://119.78.100.177/qdio/handle/2XILL650/350433
作者单位[Radwan, A.; El Fakharani, A.; Younis, M. H.; Emam, A.; Fawzy, Sh] Aswan Univ, Fac Sci, Dept Geol, Aswan 81528, Egypt; [El Fakharani, A.] King Abdulaziz Univ, Fac Earth Sci, Dept Struct Geol & Remote Sensing, Jeddah 80200, Saudi Arabia; [Abbas, H.] Assiut Univ, Fac Sci, Geol Dept, Assiut 71516, Egypt
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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[J],2021,55(1):94-111.
APA Radwan, A.,El Fakharani, A.,Abbas, H.,Younis, M. H.,Emam, A.,&Fawzy, Sh.(2021).Inverted Barrovian Metamorphic Zones in the Poly-Deformed Domains of the Western Wadi Allaqi Shear Zone (South Eastern Desert, Egypt): Geochemical and Structural Constraints.GEOTECTONICS,55(1),94-111.
MLA Radwan, A.,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".GEOTECTONICS 55.1(2021):94-111.
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