Leonardo Muniz Pichel, Christopher Aiden-Lee Jackson , Frank Peel, Oriol Ferrer

The relative timing between crustal extension and salt deposition can vary spatially along passive margin salt basins as continents unzip or as the locus of extension shifts towards the embryonic ocean spreading centre. Determining the relative timing of salt deposition, rifting, and seafloor spreading is often problematic due to the diachronous nature of rifting, the ability of salt to fill pre-existing topography, and the subsequent flow and deformation of that salt. We here use 2D PSDM seismic data and structural restorations to investigate the Merluza Graben, a large rift-related depocentre located in the southern, most proximal part of the Santos Basin, Brazil along-strike of a failed spreading centre, the Abimael Ridge. The graben is defined by up to 3.5 km of base-salt relief along its basinward-bounding fault and internal base-salt horsts that are up to 1 km high. This compartmentalises deformation, producing intra-graben extensional and contraction salt structures, ramp-syncline basins, and expulsion rollovers, resulting in a remarkably different salt-tectonic structural style to that seen in the adjacent areas. We also conduct structural restorations to analyse the spatial and temporal evolution of salt-tectonic structural styles and the relationship this has to potential prolonged crustal extension in the Merluza Graben. This approach further constrains local variations in the relative timing of rifting and salt deposition, and the impact this has on salt tectonics along the margin. The results of our study can be applied to better understand the tectono-stratigraphic development of other salt-bearing rifted margins.