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 control the routes and depositions of the turbidite systems.
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.