Fournier, François, Tassy, Aurélie, Thinon, Isabelle, Münch, Philippe, Cornée, Jean-Jacques, Borgomano, Jean, Leonide, Philippe, Beslier, Marie-Odile, Fournillon, Arnaud, Gorini, Christian, Guennoc, Pol, Oudet, Julien, Rabineau, Marina, Sage, Françoise, Toullec, Renaud (2016) Pre-Pliocene tectonostratigraphic framework of the Provence continental shelf (eastern Gulf of Lion, SE France) Bulletin de la Société géologique de France, 187 (4) 187-215 doi:10.2113/gssgfbull.187.4-5.187
Reference Type | Journal (article/letter/editorial) | ||
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Title | Pre-Pliocene tectonostratigraphic framework of the Provence continental shelf (eastern Gulf of Lion, SE France) | ||
Journal | Bulletin de la Société géologique de France | ||
Authors | Fournier, François | Author | |
Tassy, Aurélie | Author | ||
Thinon, Isabelle | Author | ||
Münch, Philippe | Author | ||
Cornée, Jean-Jacques | Author | ||
Borgomano, Jean | Author | ||
Leonide, Philippe | Author | ||
Beslier, Marie-Odile | Author | ||
Fournillon, Arnaud | Author | ||
Gorini, Christian | Author | ||
Guennoc, Pol | Author | ||
Oudet, Julien | Author | ||
Rabineau, Marina | Author | ||
Sage, Françoise | Author | ||
Toullec, Renaud | Author | ||
Year | 2016 (September 1) | Volume | 187 |
Issue | 4 | ||
Publisher | EDP Sciences | ||
DOI | doi:10.2113/gssgfbull.187.4-5.187Search in ResearchGate | ||
Generate Citation Formats | |||
Mindat Ref. ID | 530855 | Long-form Identifier | mindat:1:5:530855:6 |
GUID | 0 | ||
Full Reference | Fournier, François, Tassy, Aurélie, Thinon, Isabelle, Münch, Philippe, Cornée, Jean-Jacques, Borgomano, Jean, Leonide, Philippe, Beslier, Marie-Odile, Fournillon, Arnaud, Gorini, Christian, Guennoc, Pol, Oudet, Julien, Rabineau, Marina, Sage, Françoise, Toullec, Renaud (2016) Pre-Pliocene tectonostratigraphic framework of the Provence continental shelf (eastern Gulf of Lion, SE France) Bulletin de la Société géologique de France, 187 (4) 187-215 doi:10.2113/gssgfbull.187.4-5.187 | ||
Plain Text | Fournier, François, Tassy, Aurélie, Thinon, Isabelle, Münch, Philippe, Cornée, Jean-Jacques, Borgomano, Jean, Leonide, Philippe, Beslier, Marie-Odile, Fournillon, Arnaud, Gorini, Christian, Guennoc, Pol, Oudet, Julien, Rabineau, Marina, Sage, Françoise, Toullec, Renaud (2016) Pre-Pliocene tectonostratigraphic framework of the Provence continental shelf (eastern Gulf of Lion, SE France) Bulletin de la Société géologique de France, 187 (4) 187-215 doi:10.2113/gssgfbull.187.4-5.187 | ||
In | (2016, September) Bulletin de la Société géologique de France Vol. 187 (4) EDP Sciences | ||
Abstract/Notes | Abstract The seaward extension of onshore formations and structures were previously almost unknown in Provence. The interpretation of 2D high-resolution marine seismic profiles together with the integration of sea-bottom rock samples provides new insights into the stratigraphic, structural and paleogeographic framework of pre-Messinian Salinity Crisis (MSC) deposits of the Provence continental shelf. Seven post-Jurassic seismic units have been identified on seismic profiles, mapped throughout the offshore Provence area and correlated with the onshore series. The studied marine surface and sub-surface database provided new insights into the mid and late Cretaceous paleogeography and structural framework as well as into the syn- and post-rift deformation in Provence. Thick (up to 2000 m) Aptian-Albian series whose deposition is controlled by E-W-trending faults are evidenced offshore. The occurrence and location of the Upper Cretaceous South-Provence basin is confirmed by the thick (up to 1500 m) basinal series downlaping the Aptian-Albian unit. This basin was fed in terrigenous sediments by a southern massif (“Massif Méridional”) whose present-day relict is the Paleozoic basement and its sedimentary cover from the Sicié imbricate. In the bay of Marseille, thick syn-rift (Rupelian to Aquitanian) deposition occurred (>1000 m). During the rifting phase, syn-sedimentary deformations consist of dominant N040 to N060 sub-vertical faults with a normal component and N050 drag-synclines and anticlines. The syn-rift and early post-rift units (Rupelian to early Burdigalian) are deformed and form a set of E-W-trending en echelon folds that may result from sinistral strike-slip reactivation of N040 to N060 normal faults during a N-S compressive phase of early-to-mid Burdigalian age (18–20 Ma). Finally, minor fault reactivation and local folding affect post-rift deposits within a N160-trending corridor localized south of La Couronne, and could result from a later, post-Burdigalian and pre-Pliocene compressive phase. |
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