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• W2072035494 startingPage "298" @default.
• W2072035494 abstract "A depositional model of the lower Pliocene Hagul formation, which is exposed in the East Cairo district (Egypt), is proposed with more than 10 depositional cycles recognized. Field occurrence, detailed petrographic investigation and geochemical analysis revealed that the sediments within each cycle are the result of three sequential sedimentological processes: (1) alluvial sedimentation, (2) calcretization, and (3) precipitation of palustrine carbonate. It was concluded that Hagul formation has been deposited within the distal part of an alluvial plain during three successive climatic conditions: a humid climate during which alluvial sediments were deposited, a semi-arid climate with episodic precipitation which was favorable for pedogenic calcrete development, and a sub-humid climate during which groundwater level was gradually elevated and groundwater calcrete accumulated. Rising groundwater level continued until shallow wetlands covered the area and palustrine limestone was precipitated. Variations in the thickness and the nature of the host sediment, calcrete and palustrine limestone cycle suggest that each of the sedimentation processes varied from cycle to cycle." @default.
• W2072035494 created "2016-06-24" @default.
• W2072035494 creator A5004968469 @default.
• W2072035494 creator A5083953206 @default.
• W2072035494 date "2008-08-01" @default.
• W2072035494 modified "2023-09-23" @default.
• W2072035494 title "Occurrence of cyclic palustrine and calcrete deposits within the lower Pliocene Hagul formation, East Cairo district, Egypt" @default.
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• W2072035494 doi "https://doi.org/10.1016/j.jafrearsci.2008.01.009" @default.
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