Interstratified vermiculite–mica in the gneiss–metapelite–serpentinite rocks at Hafafit area, Southern Eastern Desert, Egypt: From metasomatism to weathering

Author:

Harraz H.Z.,Hamdy M.M.

Publisher

Elsevier BV

Subject

Earth-Surface Processes,Geology

Reference87 articles.

1. Geochemical constraints from the Hafafit Metamorphic Complex (HMC): evidence of neoproterozoic back-arc basin development in the central Eastern Desert of Egypt;Abd El-Naby;Journal of African Earth Sciences,2006

2. Tectono-metamorphic evolution of the Wadi Hafafit Culmination (central Eastern Desert, Egypt). Implication for neoproterozoic core complex exhumation in NE Africa;Abd El-Naby;Geologica Acta,2008

3. Anthophyllite–vermiculite deposit of Hafafit, Eastern Desert, Egypt;Amin;Economic Geology,1954

4. Kyanite in quartz segregations in the central Eastern Desert, Egypt;Awad;Egyptian Mineralogist,1994

5. Nature and origin of an aluminous vermiculitic weathering products in acid soils from upland catchments in Scotland;Bain;Clay Minerals,1990

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