Event-Stratification in Nummulite Accumulations and in Shell Beds from the Eocene of Egypt

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URI: http://nbn-resolving.de/urn:nbn:de:bsz:21-opus-40075
http://hdl.handle.net/10900/49304
Dokumentart: (wissenschaftlicher) Artikel
Date: 1992
Language: German
Faculty: 7 Mathematisch-Naturwissenschaftliche Fakultät
Department: Geographie, Geoökologie, Geowissenschaft
DDC Classifikation: 550 - Earth sciences
Keywords: Eozän , Ägypten
License: Publishing license excluding print on demand
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Inhaltszusammenfassung:

The Eocene of Egypt comprises shallow-marine and marginal Sediments that were deposited in narrow and elongated tectonic basins forming embayments of the Tethys. Early and Middle Eocene were times of carbonate Sedimentation, but due to regression, Sediments became essentially terrigenous from the Late Eocene onwards. Compilations on stratigraphy and Sedimentation patterns are provided by SAID (1962) and SALEM (1976). The object of this paper is to apply the concept of "event-stratification" to two rather different kinds of shell deposits: 1. Accumulations of nummulites as a very special case of bioclastics. 2. Several prominent and laterally persistent shell beds, that are being used for refined stratigraphic correlation (STROUGO 1977).

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