Quantitative analyses of the spatial distribution of supercritical-flow deposit (SFD) reaveals a new proxy for paleoenvironment reconstructions and fundamental insights into the formation processes of turbidites in deep-marine settings.
We have re-evaluated the famous Annot Sandstone (where the Bouma sequence was defined) in terms of flow criticality. The results revealing advanced process-understanding of deep-marine depositional environments are now published in Terra Nova
Quantitative analyses of the spatial distribution of supercritical-flow deposit (SFD) reaveals a new proxy for paleoenvironment reconstructions and fundamental insights into the formation processes of turbidites in deep-marine settings.