Maastrichtian to Paleocene facies evolution and Cretaceous/Tertiary boundary in Middle and Southern Egypt

Autores/as

  • Peter Luger Technische Universität Berlin       

DOI:

https://doi.org/10.7203/sjp.25161

Palabras clave:

Maastrichtian, Paleocene, transgressive/regressive cycles, facies, KIT Boundary, Gebel Qreiya, southern Egypt, G. eugubina Zone

Resumen

The sedimentary history and facies development of southern Egypt during the Latest Cretaceous and Early Paleogene is summarized. The G. eugubina Zone is reported for the first time from middle Egypt, where the conglomerate usually marking a disconformity at the Cretaceous/Tertiary boundary, is absent. The Uppermost Maastrichtian strata are attributed to the M. prinsii Zone, the Late Maastrichtian index foraminifer Abathomphalus mayaroensis (Bolli) was not recovered in the investigated samples.

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Publicado

2022-09-02

Cómo citar

Luger, P. (2022). Maastrichtian to Paleocene facies evolution and Cretaceous/Tertiary boundary in Middle and Southern Egypt. Spanish Journal of Palaeontology, 3(2), 83–90. https://doi.org/10.7203/sjp.25161
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