Anatomy of a mountain: The Thebes Limestone Formation (Lower Eocene) at Gebel Gurnah, Luxor, Nile Valley, Upper Egypt
| Autor: | Marie-Pierre Aubry, Chris King, Wael Fathi Galal, Jean-Marc Baele, Robert O. B. Knox, William A. Berggren, Christian Dupuis |
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| Rok vydání: | 2017 |
| Předmět: |
010506 paleontology
Carbonate platform Lithology Micropaleontology Geology 010502 geochemistry & geophysics 01 natural sciences Deposition (geology) Sedimentary depositional environment Paleontology chemistry.chemical_compound chemistry Section (archaeology) Carbonate Sequence stratigraphy 0105 earth and related environmental sciences Earth-Surface Processes |
| Zdroj: | Journal of African Earth Sciences. 136:61-108 |
| ISSN: | 1464-343X |
| DOI: | 10.1016/j.jafrearsci.2017.05.008 |
| Popis: | We present a detailed geologic study of the Thebes Formation at Gebel Gurnah in its locus typicus on the West Bank (opposite Luxor) of the Nile River in the Upper Nile Valley, Egypt. This is the first detailed measurement and lithologic description of the ∼340 m thick (predominantly) carbonate section. The Thebes Formation is divided into thirteen major lithic units (A to M). We interpret data on the lithologic succession and variations, whole rock/clay mineralogy, and macro/micropaleontology in terms of deposition on a shallow carbonate platform episodically influenced by continental runoff, and describe six depositional sequences that we place in the global framework of Lower Eocene (Ypresian) sequence stratigraphy. We note however significant incompatibilities between the Thebes depositional sequences and the global sequences. We emend the definition of the Thebes Formation by defining its top as corresponding to level 326 m at the top of Nodular Limestone ‘L’ (NLL), and assigning the overlying beds to the Minia Limestone Formation. New biostratigraphic data and revision of previous studies establish the direct assignment of the Thebes Formation to planktonic foraminiferal Zones E4/P6b (upper part), E5/P7 and (indirectly) Zone E6/P8, and (probably, indirectly) Zone E7a/”P9”, and to calcareous nannofossil Zone NP12 and lower Zone NP13 of the Lower Eocene (Ypresian) and provide a temporal framework spanning ∼ 2.8 Myr from |
| Databáze: | OpenAIRE |
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