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 seismic data to show depocentres record minibasin subsidence dynamics and associated salt weld processes. And depocentres can migrate along‐ and across‐strike under the control of salt weld.