“…The dominance of horizontal to low-angle stratification, the sheet-like character with sharp top and basal contacts and the overall lack of fine material are interpreted to represent sheetflood fluvial deposition during repeated discharge events (Miall, 1977(Miall, , 1996(Miall, , 2006Fisher et al, 2008;Anderson et al, 1999). No clear erosive bases or higher angle crossbed sets which would point to deep, confined channels were recognised, and deposition in a non-confined braided river system is inferred (Miall, 1977(Miall, , 1996(Miall, , 2006Bridge, 1993;Bridge, 2003Bridge, , 2006.…”