Quaternary evolution of the Marrakech High Atlas and morphotectonic evidences of the Tizi N'Test Fault activity, Morocco

Autor: Delcaillau , B., Laville , E., Amhrar , M., Namous , M., Dugué , O., Pedoja , K.

Publikováno v: Geomorphology
Geomorphology, Elsevier, 2010, 118 (3-4), pp.262-279. ⟨10.1016/j.geomorph.2010.01.006⟩
Geomorphology, Elsevier, 2010, 118 (3-4), pp.262-279. 〈10.1016/j.geomorph.2010.01.006〉

International audience; Here, we consider the Ourika and Rheraia drainage basins on the Tizi NTest Fault zone in the mountains of the Marrakech High Atlas (western Morocco) with regard to Late Pleistocene tectonic activity. New insights into geomorph

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=dedup_wf_001::ed05476229e3a7ed80a399a8f768b792
https://hal.archives-ouvertes.fr/hal-01002495