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Metapelites are exposed at Wadi Ba’ba, east of Abu Zenima city; represent the northwestern extension of the Fieran-Solaf Metamorphic Complex, Sinai Peninsula, Egypt. The metapelites are characterized by qtz + pl (An(24-28)) + bt + grt +/- crd +/- sil mineral assemblage, indicating upper amphibolite facies with peak metamorphic conditions of 700 degrees C and pressures of 7 kbar, as determined by conventional geothermobarometeric methods. This resulted in incipient migmatization, forms patches of leucosomes and melanosomes. Geochemical investigation indicates that the precursor sediments of the metapelites had been deposited as immature Fe-rich shales from source materials of dominantly intermediate composition. Source area exhibited weak to moderate chemical weathering in a tectonically active continental marginal basin within a continental-arc system. A strong shallow-dipping foliation, characterizing the metapelites, was folded around an open antiform with sub-horizontal south plunging hinge.

Phase equilibria calculations in the KFMASH system indicate that the peak metamorphic conditions formed at 730-750 degrees C and 6.8-7.9 kbar. This was followed by a retrogression formed at 770-785 degrees C and 3.9-4.5 kbar. Hence, this implies an isothermal decompression and rapid exhumation of the metapelites from depth (25-29 km) in the lower crustal level at peak conditions, continuous to include shallow to middle crustal level (14-17 km), at overprint retrograde conditions. Subsequent isobaric cooling took place at 720-750 degrees C and 3.6-4.5 kbar. The resulting isothermal decompression followed by isobaric cooling clockwise P-T path of the metapelites is more likely, in which the high-temperatures attained maximum conditions during isothermal decompression were enhanced by heat flux, due to the presence of an active magmatic arc that formed on top of subducting young lithosphere. This is supported by a moderate geothermal gradient of 27-43 degrees C/km and dating compatibility of the Sinai granitoids and the metamorphic complexes. The P-T path segment records the tectonothermal histories of crustal thickening as a result of the East and West Gondwana collision at the metamorphic peak. This was subsequent by extensional and crustal thinning with syn-metamorphic magmatic intrusions, during P-T path retrogression, which resulted in the final assembly of the Arabian-Nubian Shield during Neoproterozoic. (C) 2010 Elsevier Ltd. All rights reserved.