Agnès Maillard

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The Messinian Salinity Crisis (MSC) drastically affected the physiography, morphology and sedimentation all along the Mediterranean area at the end of the Miocene. This paper presents an analysis of the effects of the MSC on the Catalan continental margin, based on a broad database of seismic reflection profiles from the oil industry and academy. We study(More)
  • Agnès Maillard, Virginie Gaullier, Bruno C. Vendeville, Francis Odonne
  • 2003
Detailed mapping of the Ligurian-Provençal Basin (northwestern Mediterranean) indicates that salt diapirs in the deep basin are restricted to an area whose upslope boundary forms reentrants located above deep crustal transfer zones associated with the opening of the basin in Oligo–Miocene times. Because these basement faults were no longer active in(More)
We present the structure and evolution of the eastern part of the Demerara plateau, offshore French Guiana, from the analysis of geophysical data collected during GUYAPLAC cruise. This area is located at the intersection of a transform segment and a divergent segment of a continental margin related to the Early Cretaceous opening of the Equatorial Atlantic.(More)
We present the structure and evolution of the eastern part of the Demerara plateau, offshore French Guiana, from the analysis of geophysical data collected during GUYAPLAC cruise. This area is located at the intersection of a transform segment and a divergent segment of a continental margin related to the Early Cretaceous opening of the Equatorial Atlantic.(More)
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