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- W2891036595 abstract "L'Argile des Milles is middle oligocene in age. It is made up of detrital elements of south western origin, set free by the destruction of soils and, later, by the erosion of the andalosite bearing cristalline continent still located south west of the Golfe du Lyon. This formation is missing in the bassin de Marseille ; this fact probably demonstrates that this basin did not exist during this period. The subsidence must have starting progressively at the beginning of the upper Oligocene, and must have become major movements during the middle Chattian. A relationship may be tentatively proposed between these facts and the drift of Sardaigne." @default.
- W2891036595 created "2018-09-27" @default.
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- W2891036595 date "1977-01-01" @default.
- W2891036595 modified "2023-09-26" @default.
- W2891036595 title "Le bassin oligocène de Marseille : stratigraphie, évolution paléogéographique" @default.
- W2891036595 doi "https://doi.org/10.3406/geolm.1977.987" @default.
- W2891036595 hasPublicationYear "1977" @default.
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