Les dépôts quaternaires, carte géologique de la France, feuille Aubagne-Marseille 3e édition

Les dépôts quaternaires, carte géologique de la France, feuille Aubagne-Marseille 3e éditio

Les dépôts quaternaires, carte géologique de la France, feuille Aubagne-Marseille 3e édition

Les dépôts quaternaires, carte géologique de la France, feuille Aubagne-Marseille 3e éditio

Les dépôts quaternaires, carte géologique de la France, feuille Aubagne-Marseille 3e édition

Les dépôts quaternaires, carte géologique de la France, feuille Aubagne-Marseille 3e éditio

Les formations post-oligocènes in notice de la carte géologique de la France

Les formations post-oligocènes in notice de la carte géologique de la Franc

Les formations post-oligocènes in notice de la carte géologique de la France

Les formations post-oligocènes in notice de la carte géologique de la Franc

Les formations post-oligocènes in notice de la carte géologique de la France

Les formations post-oligocènes in notice de la carte géologique de la Franc

Evidence for an intra-Oligocene compressive event in the Marseille-Aubagne basins (SE France)

International audienceAn Oligocene tectonic event has been suspected as the origin of thrusts and folds in several Oligocene troughs and basins of Provence, including the Marseille-Aubagne basins. Deformations are generally assumed to be to a post Oligocene extensional event. The Marseille-Aubagne basins are geographically and stratigraphically separated into three basins (Jarret, Prado and Aubagne) with each of them exhibiting their own sedimentary succession. However, each of the successions includes two main units: - The lower unit which includes several formations attributed to the Rupelian age. All of these sediments are strongly or slightly deformed depending on their location with respect to the main faults. - The upper unit which includes formations of mainly Chattian age. They are undeformed or slightly deformed. Geological sections across the southern Prado basin show a succession of anticlines and synclines. Additionally the thrusting of the Carpiagne massif over the Prado basin has been evidenced since 1952. These deformations are here related to a compressional event According to palaeontological data, the latest deformed strata are ascribed to the Late Rupelian, whereas the earliest undeformed strata are ascribed to the Latest Rupelian. This is in accordance with age determinations on detrital zircons extracted from the latest deformed sandstone, and from the youngest age of detrital zircons from the undeformed sandstone. Thus, the stratigraphic limit between the deformed and undeformed formations should be set around the Rupelian / Chattian limit (28.1 Ma) according to the latest chronostratigraphic chart. Finally, we discuss correlations with similar events occurring around the Mediterranean area