We use high quality 3D seismic to document and analysize the evolution of a turbidite system and its interaction with salt-related structures. We show that the growth and decay of salt related structures result in variations in seafloor topography which ultimately controls the routes and depositions of the turbidte system.
We use high quality 3D seismic to document the evolution of a network of minibasins and their associated salt-related structures. We show that minibasin initiation and subsequent evolution can be controlled by different mechanisms and therefore categorising minibasins into simple domain-related types is problematic.
We use high quality 3D seismic dataset to demonstarte the interaction between large-scale rift architecture (rift segment vs rift accommodation zone) and complex pre-rift salt-related structures.
We use seismic data to study the structural style and kinematic evolution of the Jequitinhonha Basin, Brazil.