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- W2080759216 abstract "Un nouvel âge vient d'être obtenu par la méthode de gradedation dans les marnes de la Grenette, formation la plus représentative du Burdigalien du bassin de Crest. Il est de 17,4±0,15 M.a., ce qui la date de la partie supérieure de l'étage pris dans son sens large actuel. Ceci met cette formation en équivalence avec une partie au moins des marnes bleues de Faucon, du stratotype du bassin de Valréas. Outre son intérêt dans les corrélations régionales, ce résultat indique un fonctionnement sédimentaire un peu plus tardif dans ce secteur effectivement plus septentrional et précise ainsi les modalités de la transgression miocène dans le sillon périalpin. By the method of grade-dating, in the “marls of la Grenette”—themost representative formation of the Burdigalian of the Crest basin—a new age has just been found out. It is 17,4±0,15 M.a., which situates them in the upper part of the stage, in the wide meaning of nowadays. As a result they can be considered as equivalent at least to a part of the “blue marls of Faucon”, from the stratotype of the basin of Valréas. Besides its interest in regional correlations, this result shows a rather late sedimentary activity in this sector, which is actually situated to the north of Valréas, and clarifies the modes of the miocene transgression in the perialpine groove." @default.
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- W2080759216 date "1989-01-01" @default.
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- W2080759216 title "Grade-datation dans le Burdigalien du bassin de Crest(Drôme, moyenne Vallée du Rhône): Comparaison avec le stratotype rhodanien" @default.
- W2080759216 cites W2069382153 @default.
- W2080759216 doi "https://doi.org/10.1016/s0016-6995(89)80137-8" @default.
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