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pro vyhledávání: '"Mostapha Bachaoui"'
Publikováno v:
Journal of African Earth Sciences. 120:198-207
The High Atlas is a 100 km wide zone defined by E-W to NE-SW trending folds nearly orthogonal to the Atlantic coastline. The major compressional structures in the High Atlas consist of large-scale fold systems which affect Mesozoic and Cainozoic form
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::060171b78edd157a3edbef76a83b6aa5
https://doi.org/10.1016/j.jafrearsci.2016.05.009
https://doi.org/10.1016/j.jafrearsci.2016.05.009
