The Wadi EI-Hudi area, in the south Eastern Desert of Egypt, comprises a highgrade metamorphic complex of migmatite and biotite gneiss that host a garnet-bearing leucogrenite body. This complex has been intruded later by post-orogenic pink granites. Gneisses and migmatites show obvious irregular lay
Experimental evidence bearing on the stability of monazite during crustal anaatexis
✍ Scribed by Robert P. Rapp; F. J. Ryerson; Calvin F. Miller
- Book ID
- 111897403
- Publisher
- American Geophysical Union
- Year
- 1987
- Tongue
- English
- Weight
- 355 KB
- Volume
- 14
- Category
- Article
- ISSN
- 1944-8007
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