Recognition of cyclic steps in sandy and gravelly turbidite sequences, and consequences for the Bouma facies model

Postma, George; Kleverlaan, Kick; Cartigny, Matthieu J.B.. 2014 Recognition of cyclic steps in sandy and gravelly turbidite sequences, and consequences for the Bouma facies model. Sedimentology, 61 (7). 2268-2290. 10.1111/sed.12135

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Official URL: http://dx.doi.org/10.1111/sed.12135

Abstract/Summary

Preservation of cyclic steps contrasts markedly with that of subcritical-flow bedforms, because cyclic steps migrate upslope eroding their lee face and preserving their stoss side. Such bedforms have not been described from turbidite outcrops and cores as yet. A conceptual block diagram for recognition of cyclic steps in outcrop has been constructed and is tested by outcrop studies of deep water submarine fan deposits of the Tabernas Basin in south-eastern Spain. Experimental data indicate that depositional processes on the stoss side of a cyclic step are controlled by a hydraulic jump, which decelerates the flow and by subsequent waxing of the flow up to supercritical conditions once more. The hydraulic jump produces a large scour with soft-sediment deformation (flames) preserved in coarse-tail normal-graded structureless deposits (Bouma Ta), while near-horizontal, massive to stratified top-cut-out turbidite beds are found further down the stoss side of the bedform. The architecture of cyclic steps can best be described as large, up to hundreds of metres, lens-shaped bodies that are truncated by erosive surfaces representing the set boundaries and that consist of nearly horizontal lying stacks of top-cut-out turbidite beds. The facies that characterize these bedforms have traditionally been described as turbidite units in idealized vertical sequences of high-density turbidity currents, but have not yet been interpreted to represent bedforms produced by supercritical flow. Their large size, which is in the order of 20 m for gravelly and up to hundreds of metres for sandy steps, is likely to have hindered their recognition in outcrop so far.

Item Type:	Publication - Article
Digital Object Identifier (DOI):	10.1111/sed.12135
ISSN:	00370746
Additional Keywords:	Bouma sequence; cyclic steps; high-density turbidity current; hydraulic jump; supercritical-flow bedforms; traction carpet; turbidite facies
Date made live:	05 Aug 2014 11:02 +0 (UTC)
URI:	https://nora.nerc.ac.uk/id/eprint/508018

Item Type:

Publication - Article

Digital Object Identifier (DOI):

10.1111/sed.12135

ISSN:

00370746

Additional Keywords:

Bouma sequence; cyclic steps; high-density turbidity current; hydraulic jump; supercritical-flow bedforms; traction carpet; turbidite facies

Date made live:

05 Aug 2014 11:02 +0 (UTC)

URI:

https://nora.nerc.ac.uk/id/eprint/508018