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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

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Reference TypeJournal (article/letter/editorial)
TitlePre-Pliocene tectonostratigraphic framework of the Provence continental shelf (eastern Gulf of Lion, SE France)
JournalBulletin de la Société géologique de France
AuthorsFournier, FrançoisAuthor
Tassy, AurélieAuthor
Thinon, IsabelleAuthor
Münch, PhilippeAuthor
Cornée, Jean-JacquesAuthor
Borgomano, JeanAuthor
Leonide, PhilippeAuthor
Beslier, Marie-OdileAuthor
Fournillon, ArnaudAuthor
Gorini, ChristianAuthor
Guennoc, PolAuthor
Oudet, JulienAuthor
Rabineau, MarinaAuthor
Sage, FrançoiseAuthor
Toullec, RenaudAuthor
Year2016 (September 1)Volume187
Issue4
PublisherEDP Sciences
DOIdoi:10.2113/gssgfbull.187.4-5.187Search in ResearchGate
Generate Citation Formats
Mindat Ref. ID530855Long-form Identifiermindat:1:5:530855:6
GUID0
Full ReferenceFournier, 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 TextFournier, 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/NotesAbstract
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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