The Nile Cone: Submarine fan development by cyclic sedimentation |
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Authors: | Andrés Maldonado Daniel Jean Stanley |
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Institution: | 1. Sección de Estratigrafía, Instituto “Jaime Almera”, C.S.I.C., Barcelona Spain;2. Division of Sedimentology, Smithsonian Institution, Washington, D.C. U.S.A. |
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Abstract: | The Quaternary sections of the Nile Cone in the eastern Mediterranean are formed by regionally extensive repetitions of sediment sequences (cyclothems s.l.) showing a successive, orderly arrangement of sediment types. Detailed lithofacies analysis reveals the recurrence of three basic terms in many cores: a basal olive-gray hemipelagic mud and turbidite sequence; a middle sapropel sequence; and an upper yellowish-orange hemipelagic sequence, including calcareous ooze, and a turbiditic sequence. This cyclic sedimentation closely reflects the Quaternary dynamics. The development of the Nile submarine fan in an enclosed, silled basin has resulted in a particularly close relation between biogenic-terrigenous depositional patterns and climatic and oceanographic factors affecting the Mediterranean. |
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