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Structural data collected along the range argue for an Eocene Noshorten- ing event. The age of this shortening event is constrained Airis N290 the fact that faulting and folding affect the Late Creta- ceous-Paleocene continental deposits along the Airis N290 flank of the La Nerthe range and is sealed by the Miocene marine deposits.

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Moreover striated fault planes display both horizontal and vertical striae suggesting that they were re- activated during the Oligocene Airis N290 event. We question here the shortening directions Airis N290 the Southern Pro- vence thrust belt. During the Eocene the Provence area was in the foreland of a complex orogenic belt that extended from the Betic Cordillera to the Corsica-Sardinia block.

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This orogenic belt developed along the subduction linked to the convergence between Africa and Eurasia. Although the convergence vector was nearly N-S the NE-SW orientation of the trench may have led to a complex deformation pattern along the orogenic belt with NW-SE and N-S shortening directions that reflected both the along-trench Airis N290 and Airis N290 regional convergence.

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Airis N290 Pyrenees-Provence belt and the Alps were both ac- tive in the late Eocene. In spite of many works the eastward termination of the so-called Pyrenean belt and its connection to the Alps in the Provence-Corsica-Sardinia area during the late Eocene is still a matter of debate.

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We discuss in this paper the Eocene geometry and kine- matics Airis N290 the Southern Provence fold-and-thrust belt. Struc- tural data collected along three distinct areas indicate a Bull.

The enclosed region indicates the location of the Provence area fig. Abre- Airis N290 Alpine Corsica, CPA: Calabro-Peloritan arc, CR: Catalan ranges. Le cadre indique la localisation de la Provence fig.

Corse al- pine,CPA: Arc calabro-peloritain, CR: Emails and Electronic Communication We offer you to subscribe to our newsletters. If Airis N290 no longer wish to receive correspondence, emails, or other communications from us, you may opt-out.

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