Distinguishing dense-to-dilute and dilute- to-dense flow transformation: criteria from Permo–Triassic deep-water deposits offshore mid-Norway

Flow transformation of subaqueous particulate gravity currents takes place when there is a change of sediment transport mechanisms, and transformation can be both from dense-to-dilute flow, and from dilute-to-dense flow, where each consists of a continuum of processes. As a result, deposits of transforming flows can contain characteristics of both debrites and turbidites. The resulting […]