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Anatomy of a mountain: the Thebes Limestone Formation (Lower Eocene) at Gebel Gurnah, Luxor, Nile Valley, Upper Egypt
King, C.; Dupuis, C.; Aubry, M.-P.; Berggren, W.A.; Knox, R.O.'B.; Galal, W.F.; Baele, J.-M. (2017). Anatomy of a mountain: the Thebes Limestone Formation (Lower Eocene) at Gebel Gurnah, Luxor, Nile Valley, Upper Egypt. J. Afr. Earth Sci. 136: 61-108. https://dx.doi.org/10.1016/j.jafrearsci.2017.05.008
In: Journal of African Earth Sciences. Elsevier: Oxford & Amsterdam. ISSN 1464-343X; e-ISSN 1879-1956, meer
Peer reviewed article  
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Author keywords
    Thebes Limestone; Lower Eocene; Gebel Gurnah; Egypt; Sequencestratigraphy
Auteurs  Top 
  • King, C.
  • Dupuis, C., meer
  • Aubry, M.-P.
  • Berggren, W.A.
  • Knox, R.O.'B.
  • Galal, W.F.
  • Baele, J.-M., meer
Abstract
    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 similar to 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 similar to 2.8 Myr from <52.45 to similar to 49.6 Ma for the deposition of the Thebes Formation prior to the prominent sea level fall (similar to 49.6 Ma) towards the end of the Early Eocene. Dominantly carbonate deposition, with a strongly reduced detrital influx, occurred on a very wide shelf (probably) at least similar to 100 km from the coastline. The thick sedimentary succession and the marked vertical lithologic variations are interpreted as resulting from sea level fluctuations imprinted on a long-term decrease in sea-level associated with rapid subsidence reflecting tectonic relaxation after the major Late Paleocene tectonic reorganization of the Syrian Arc.
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