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Depositional environment of the Upper Cretaceous oil shales in the Negev Desert, Israel: Geochemical constraints based on trace elements and stable isotopes

Illner, Peter

A study in inorganic geochemistry from the Campanian (Mishash Formation) - Maastrichtian (Ghareb Formation) transition of southern Israel was done to provide insights into the inference of foraminiferal assemblages, water column-oxygen levels, trace metal enrichment on a high-productivity seafloor. A series of high-resolution approaches in inorganic geochemistry applied on a 50 m sequence in the Efe`s syncline of the Negev desert. A conceptual model of the deposition history was developed.

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Volltext §
DOI: 10.5445/IR/1000046212
Zugehörige Institution(en) am KIT Institut für Mineralogie und Geochemie (IMG)
Publikationstyp Hochschulschrift
Jahr 2014
Sprache Englisch
Identifikator urn:nbn:de:swb:90-462122
KITopen-ID: 1000046212
Verlag KIT, Karlsruhe
Abschlussart Dissertation
Fakultät Fakultät für Bauingenieur-, Geo- und Umweltwissenschaften (BGU)
Institut Institut für Mineralogie und Geochemie (IMG)
Prüfungsdaten 16.07.2014
Referent/Betreuer Prof. T. Neumann
Schlagworte Anoxia, foraminifera, trace element, sulphur isotopy, Campanian-Maastrichtian transition
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