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- W2759633532 abstract "Abstract All the Neocomian outcrops in the western Ouarsenis region, Algeria, represent parts of a nappe formed by gravitational sliding of lower Cretaceous shaly limestone masses. The Tell region has been identified as the source of the masses." @default.
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- W2759633532 date "1956-01-01" @default.
- W2759633532 modified "2023-10-17" @default.
- W2759633532 title "Le Cretace inferieur dans l'Ouarsenis occidental; tectonique, paleogeographie" @default.
- W2759633532 doi "https://doi.org/10.2113/gssgfbull.s6-vi.7-9.909" @default.
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