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- W2065438050 abstract "The Early Carboniferous sediments of the North-East of the Moroccan western Meseta are very diversified. They contain numerous types of carbonates, deposited upon shallow shelves, as well as deeper gravity and hemipelagic deposits. The progressive Early Carboniferous transgression, starts from the Agouraï area at V2a and reaches Imouzzer of Kandar at V3bγ. The opening of the North-East of the western Meseta basin by strike-slip NE–SW faults, is V2a in age. This basin evolved in an extensive context during all of the Early Carboniferous. These sediments were stricken by a compressive deformation between the Late Namurian and Permian times.Les sédiments du Carbonifère inférieur du Nord-Est de la Méséta occidentale marocaine sont très diversifiés. Ils comprennent des dépôts carbonatés de plates-formes peu profondes, des dépôts gravitaires et des hémipélagites. La transgression du Carbonifère inférieur est progressive, elle débute au V2a à Agouraï et atteint Imouzzer du Kandar au V3bγ. Le bassin du Nord-Est de la Méséta occidentale s'est ouvert au V2a par des failles décrochantes de direction NE–SW. Il a évolué dans une ambiance extensive durant tout le Carbonifère inférieur. Ces sédiments ont été affectés par une déformation compressive post-namurienne et anté-permienne." @default.
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- W2065438050 date "1963-12-01" @default.
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- W2065438050 title "Réponse aux commentaires sur “electrical resistance of hydrogen-charged iron wires”" @default.
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- W2065438050 doi "https://doi.org/10.1016/0001-6160(63)90038-5" @default.
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