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

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dc.contributor.author Aigner, Thomas de_DE
dc.date.accessioned 2009-06-19 de_DE
dc.date.accessioned 2014-03-18T10:20:13Z
dc.date.available 2009-06-19 de_DE
dc.date.available 2014-03-18T10:20:13Z
dc.date.issued 1992 de_DE
dc.identifier.other 307682161 de_DE
dc.identifier.uri http://nbn-resolving.de/urn:nbn:de:bsz:21-opus-40075 de_DE
dc.identifier.uri http://hdl.handle.net/10900/49304
dc.description.abstract 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). de_DE
dc.language.iso de de_DE
dc.publisher Universität Tübingen de_DE
dc.rights ubt-podno de_DE
dc.rights.uri http://tobias-lib.uni-tuebingen.de/doku/lic_ohne_pod.php?la=de de_DE
dc.rights.uri http://tobias-lib.uni-tuebingen.de/doku/lic_ohne_pod.php?la=en en
dc.subject.classification Eozän , Ägypten de_DE
dc.subject.ddc 550 de_DE
dc.title Event-Stratification in Nummulite Accumulations and in Shell Beds from the Eocene of Egypt en
dc.type (wissenschaftlicher) Artikel de_DE
utue.publikation.fachbereich Geographie, Geoökologie, Geowissenschaft de_DE
utue.publikation.fakultaet 7 Mathematisch-Naturwissenschaftliche Fakultät de_DE
dcterms.DCMIType Text de_DE
utue.publikation.typ article de_DE
utue.opus.id 4007 de_DE

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