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- W2033597907 abstract "Fifteen hiatuses of the first order have been shown to exist in the Palaeogene of the Paris Basin, in relation to neighbouring basins, the eustatic curve, and breaks in ocean-bottom sedimentation. In the neritic and continental domains there are very frequent and very long second order or intraformational hiatuses which separate sequences of sedimentation whose deposition represents only a short part of geological time. The data from biostratigraphy, magnetostratigraphy and chemostratigraphy shown most of the events that characterize the Palaeocene-Eocene and Eocene-Oligocene boundaries were not simultaneous and are sometimes diachronous. These boundaries are in reality transitions whose duration can exceed 1 million years; hence the difficulty of choosing a boundary-strateype for each." @default.
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- W2033597907 date "1989-01-01" @default.
- W2033597907 modified "2023-09-25" @default.
- W2033597907 title "Stratigraphy of the Palaeogene: hiatuses and transitions" @default.
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- W2033597907 doi "https://doi.org/10.1016/s0016-7878(89)80051-3" @default.
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