Gravitational collapse origin of shear zones, foliations and linear structures in the Neoproterozoic cover nappes, Eastern Desert, Egypt
AR Fowler, B El Kalioubi - Journal of African Earth Sciences, 2004 - Elsevier
The Um Esh–Um Seleimat area lies to the west of the Meatiq Core Complex (MCC), in the
Central Eastern Desert (CED), Egypt, which forms part of the Neoproterozoic Arabian–
Nubian Shield in NE Africa and Western Arabia. The study area is a NW-trending zone of
intensely foliated ophiolitic melange and molasse sedimentary rocks. There is a single
regional foliation, S1, defined mainly by low-to very low-grade metamorphic phases, though
grade increases to amphibolite facies in the areas bordering the MCC. S1 is associated with …
Central Eastern Desert (CED), Egypt, which forms part of the Neoproterozoic Arabian–
Nubian Shield in NE Africa and Western Arabia. The study area is a NW-trending zone of
intensely foliated ophiolitic melange and molasse sedimentary rocks. There is a single
regional foliation, S1, defined mainly by low-to very low-grade metamorphic phases, though
grade increases to amphibolite facies in the areas bordering the MCC. S1 is associated with …
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