Incisions are stratigraphically important in that they record
removal of previously deposited strata, and can represent sequence boundaries.
Here, Ullah et al. describe scour surfaces at the top of the Ferron Sandstone Member
(Cretaceous, Mancos Shale Formation, Henry Mountains, Utah) that include
individual channel stories. This study shows that confluence scours have
diagnostic fill facies (single set of large steep foresets) and do not produce
multi-storey sand bodies. The results, coupled with modern analog studies,
suggest that the maximum depth of confluence scours by autogenic process may
reach up to four to five times the average depth of the incoming channels. Consequently,
allogenic incised valleys (e.g., at sequence boundaries) can be defined in
ancient systems only in situations wherein the erosional relief is more than
five times average channel depth, markedly deeper than the thickest fully
preserved storys, which in a braided stream are likely to represent confluence
scour fills. Examples of autogenic modification of allogenically formed incised
valleys suggest that both allogenic forcing and autogenic feedback can act
simultaneously in fluvial systems.
Confluence scours versus incised valleys:
examples from the Cretaceous Ferron Notom delta, southeastern Utah, U.S.A.by Mohammad S. Ullah, Janok P. Bhattacharya, and William R. Dupre
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