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The Moroccan Atlas is an intracontinental chain resulted from an aborted rifting during the Mesozoic time, by an uplifting and moderate shortening during the Late Cretaceous-Cenozoic period. Several studies have highlighted the role of tectonic inver
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::1273d6ceb8abc98ec5ccbebd960ccdd0
https://doi.org/10.5194/egusphere-egu22-669
https://doi.org/10.5194/egusphere-egu22-669