The Upper Cenomanian transgression in the High Moulouya and southern middle Atlas, Morocco
In the Southern Middle Atlas of Morocco, the well-documented Marnes a gypse (Cenomanian) are overlain by the lower part of the Amghourzif Formation, dated as Upper but not uppermost Cenomanian on the basis of benthonic foraminifera of the subfamily Rhapidionininae. The upper part of the Amghourzif y...
| Main Authors: | , , , , , |
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| Format: | Journal article |
| Language: | French |
| Published: |
1998
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