2019
DOI: 10.1007/978-3-030-34193-0_9
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Numerical Analysis of Instabilities Affecting an Excavation on the High Speed Line in Northern Morocco

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Cited by 4 publications
(11 citation statements)
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“…Piezometric measures could not be realized on superposed aquifers (no selective piezometers). However, it appears that sandstone is relatively porous (n = 12%) and therefore potentially aquifers with alternating more clayey levels of pelites probably constituting the wall of these aquifers [3]. This is confirmed by the existence of many sources at the base of the excavation, at the interface between numidian sandstones and the pelites of the Tangier nappe [3].…”
Section: Hydrogeological Contextmentioning
confidence: 98%
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“…Piezometric measures could not be realized on superposed aquifers (no selective piezometers). However, it appears that sandstone is relatively porous (n = 12%) and therefore potentially aquifers with alternating more clayey levels of pelites probably constituting the wall of these aquifers [3]. This is confirmed by the existence of many sources at the base of the excavation, at the interface between numidian sandstones and the pelites of the Tangier nappe [3].…”
Section: Hydrogeological Contextmentioning
confidence: 98%
“…The excavation object of this study is located on the high-speed line between Kenitra and Tangier, specifically in the rural commune of Hjar Nhal, in the region of Tanger-Tetouan-Al Hoceima. It extends for 1170 m in length, its maximum height is 62 m at the axis [3].…”
Section: Geographical Contextmentioning
confidence: 99%
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