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Genesis and geometry of tilted blocks in the Theban Hills, near Luxor (Upper Egypt)

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dc.contributor.author Dupuis, Christian
dc.contributor.author Aubry, Marie-Pierre
dc.contributor.author King, Christopher
dc.contributor.author Knox, Robert W. O'B.
dc.contributor.author Berggren, William A.
dc.contributor.author Youssef, Mostafa
dc.contributor.author Galal, Wael Fathi
dc.contributor.author Roche, Marc
dc.date.accessioned 2011-12-27T18:29:57Z
dc.date.available 2011-12-27T18:29:57Z
dc.date.issued 2011-02-16
dc.identifier.uri http://hdl.handle.net/1912/4960
dc.description Author Posting. © The Author(s), 2011. This is the author's version of the work. It is posted here by permission of Elsevier B.V. for personal use, not for redistribution. The definitive version was published in Journal of African Earth Sciences 61 (2011): 245-267, doi:10.1016/j.jafrearsci.2011.06.001. en_US
dc.description.abstract The desertic Theban hills between the edge of the alluvial plain of the Nile and the prominent cliffs at the eastern edge of the Theban Plateau consist of imbricated tilted blocks organized in parallel groups representing successive generations of gravitational collapse structures (or slumps). The older (distal) generations correspond to low, rounded hills farther from the Theban cliffs. The youngest (proximal) generation forms higher hills with young relief. Reverse faults occur at the contact between proximal and distal tilted blocks whereas the proximal tilted blocks rest along listric faults on the substratum (Tarawan Chalk and Esna Shale Formations) and against the Theban cliffs. We hypothesize that the emplacements of the tilted blocks were related to major Pleistocene pluvial episodes, each marked by active flow of the Nile River and significant recess of the Theban cliffs. Tectonic thinning and intensive erosion of the Esna Shale Formation were determinant in shaping the Theban landscape. en_US
dc.description.sponsorship National Geographic Society for its continued support of our geological research on the Theban Mountain. en_US
dc.format.mimetype application/pdf
dc.language.iso en_US en_US
dc.relation.uri http://dx.doi.org/10.1016/j.jafrearsci.2011.06.001
dc.subject Gravitational collapse structures en_US
dc.subject Listric and reverse faults en_US
dc.subject Pleistocene pluvials en_US
dc.subject Pleistocene erosion en_US
dc.subject Tilted blocks en_US
dc.title Genesis and geometry of tilted blocks in the Theban Hills, near Luxor (Upper Egypt) en_US
dc.type Preprint en_US


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