Thermodynamic modelling of Sol Hamed serpentinite, South Eastern Desert of Egypt: Implication for fluid interaction in the Arabian–Nubian Shield ophiolites

Author:

Abu-Alam Tamer S.,Hamdy Mohamed M.

Publisher

Elsevier BV

Subject

Earth-Surface Processes,Geology

Reference127 articles.

1. Abd El-Naby, H.H., Frisch, W., 1999. Metamorphic sole of Wadi Haimur-Abu Swayel ophiolite: implications on late Proterozoic accretion. In: Wall, H.D., Greiling, R.O. (Eds.), Aspects of Pan-African Tectonics. Heidelberg, Germany, pp. 9–14.

2. Geochemistry and tectonic evolution of the Neoproterozoic incipient arc–forearc crust in the Fawakhir area, Central Eastern Desert of Egypt;Abd El-Rahman;Precambrian Res.,2009

3. Syn- and post-accretionary structures in the Neoproterozoic Central Allaqi-Heiani suture zone, Southeastern Egypt;Abdeen;Precambrian Res.,2011

4. Tectonic evolution of the Nakasib suture, Red Sea Hills, Sudan: evidence for a late Precambrian Wilson Cycle;Abdelsalam;J. Geol. Soc.,1993

5. Sutures and shear zones in the Arabian–Nubian Shield;Abdelsalam;J. Afr. Earth Sci.,1996

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