ArticleScientific reports2026
Mineral and geochemical variability of the phosphorite deposits in the Duwi Formation, Western Desert, Egypt: Insights into paleoenvironment and physicochemical conditions.
Article in Scientific reports, 2026. The graph could read no effect estimate from its abstract, so it casts no vote on the map. Not yet cited in PubMed.
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Abstract
This study explores the phosphorite deposits from the Lower Member of the Duwi Formation in Egypt, which forms part of the Mediterranean phosphorite belt extending from Africa to Asia. Detailed petrographical, mineralogical, and geochemical investigations were carried out to shed light on the prevailing physicochemical conditions and diagenetic history of these deposits. They are classified into three east-west trending belts, with significant economic occurrences located in the central facies belt, particularly along the Nile Valley and Red Sea shoreline. Geochemical analyses indicated that these phosphorites are predominantly composed of CaO (avg. 35.83 wt%) and P
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