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The sedimentology of the succession indicates that these units represent bar top and marginal deposits in a braided fluvial setting.
In all three basins, this mudstone-dominated interval passes into sandstonedominated sediments of a braided fluvial system.
It illustrates a special kind of trapping, which is produced by the collisional motion of the particles along braided magnetic lines.
The bulk of the formation consists of fluvial sand deposits, apparently deposited by braided river flow.
Nonetheless, the libretti provide invaluable information about the various woven or braided patterns combined with the round dances.
This back apron has two hanging tiers of braided leather cords, with long sliced shells attached at the bottom.
The successions represent two deepening-upward sequences, both starting as fluvial (braided river) systems and ending as shallow marine tidally dominated environments.
The remaining upper part of the unit displays a sudden change in sedimentary environment from a braided to meandering environment.
Frequent intercalations of muddy shales between the cross-bedded or laminated fine-grained sandstones exclude the interpretation of formation by a braided river system for this part of the basin.
To the sedimentary geologist, this provides an insight into the ichnofauna associated with braided river deposits and hence a further tool for the reconstruction of ancient fluvial environments.
An interesting and informative departure from the scope of most collections of sedimentology papers is the inclusion of two papers on the ecology of braided rivers.
Microlites form braided flow patterns.
The association of coarse-grained overbank facies and channel-fill sandstone facies with sheet-like body geometries indicate that this member is made up of the deposits of a braided river/braidplain system.
The pattern of upward-fining cycles is similar to that of a braided river, but the internal texture of the gravels shows that debris flow processes were dominant during deposition.
