The diagenesis of lower Eocene shallow water carbonates with flint was studied in the Gebel Rewagen area, Eastern Desert, Egypt. The carbonates are mainly wackestones to packstones with benthic bioclasts embedded in a dark red luminescent micrite matrix. The studied succession displays a complex dia
Lower Miocene stratigraphy of the Gebel Shabrawet area, north Eastern desert Egypt
β Scribed by Osman Abdelghany
- Book ID
- 108460178
- Publisher
- Elsevier Science
- Year
- 2002
- Tongue
- English
- Weight
- 619 KB
- Volume
- 34
- Category
- Article
- ISSN
- 1464-343X
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