Facies	Lithofacies code	Lithology description	Structures	Interpretation	Appearances
Fluvial	Gm	0.5 - 1 m thick, sandy matrix-supported, red brown intra-formational mudstone or grey to white-grey quartz pebbles conglomerates, pebbles are around 1 - 3 cm in diameter.	Massive to crudely bedding	Basal lag deposits	B04, B09, B10, B11
	St	0.5 - 1.5 m thick, fine to medium-grained sandstones, containing grouped or solitary sets of trough cross laminations	Trough cross-bedding	Downstream migration of sinuous-crested dunes in fluvial channels (lower flow regime)	B04, B09, B10, B11
	Sp	0.5 - 1 m thick, fine to medium-grained sandstone with solitary sets of planar cross laminations, better sorted and cleaner than St and lack mudstone or quartz pebbles	Planar cross-bedding	Transverse and linguoid sand bars in fluvial channels (lower flow regime)	B04, B09, B10, B11
	Sh	0.2 - 0.5 m thick, red-brown, fine-grained sandstones with millimetre-scaled thin laminations.	Horizontal lamination	Flash floods deposits (lower flow regime)	B04, B09, B10, B11
	Fl	0.2 - 1 m thick, argillaceous and micaceous, very fine-grained sandstones to siltstones.	Thin laminations with soft sediment deformation	Temporary floodplains and inactive or abandon channels	B04, B09, B10, B11
	Fm	0.2 - 0.5 m thick, micaceous dark red-brown silty mudstones and mudstones	Massive bedding	Overbank	B04, B09, B10, B11
Aeolian	Sps	0.5 - 1 m thick, upper fine- to medium-grained, well sorted, well rounded sandstones. High visible porosity, friable nature and the absence of muddy or conglomeratic intra-clasts.	Pin-stripe lamination	Dune	B07, B08
Aeolian	Sw	1 - 2 m thick, very fine- to medium-grained sandstones, moderately to well sorted, locally developed mud desiccation, de-water structure, cross-bedding ripples and argillaceous streaks	Discontinuous wavy lamination with several local structures	Interdune with fluctuating dry and wet conditions	B07, B08