Internal deformation of a muddy gravity flow and its interaction with the seafloor (site C0018 of IODP Expedition 333, Nankai Trough, SE Japan)

Laberg, J. S., Strasser, M., Alves, Tiago Marcos ORCID: https://orcid.org/0000-0002-2765-3760, Gao, S., Kawamura, K., Kopf, A. and Moore, G. F. 2017. Internal deformation of a muddy gravity flow and its interaction with the seafloor (site C0018 of IODP Expedition 333, Nankai Trough, SE Japan). Landslides 14 (3) , pp. 849-860. 10.1007/s10346-016-0766-7

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Abstract

The processes of flow deformation of marine mass-transport sediments, including their ability to affect the underlying substrate and add mass during sediment flow events, are addressed based on sedimentological analyses of strata from the distal part of a ∼61-m-thick mass-transport deposit (MTD 6) drilled during Integrated Ocean Drilling Program (IODP) Expedition 333. Our analyses, supported by 3D seismic data, show a cohesive density flow deformed by folding, faulting and shear, except for its lowermost part (∼7 m), where no deformation and sediment entrainment was identified. While the lowermost part moved as rigid sediment, the underlying sand layer acted as the basal shear zone for this part of the distal MTD 6. This shear zone was restricted to the sand, not involving the overlying sediments. From this, the studied part of MTD 6 was found to represent a case where the flow behaviour at least partly depended on the location and properties of the underlying sand layer, a situation that so far has received little attention in studies of marine flows. Our results also show that shear-induced mixing, located by the initial layering, is an important process in the flow transformation from cohesive slumps to mud flows and that this may occur over short distances (<4 km) without involving disintegration into blocks, probably due to only moderate prefailure consolidation of the sediments involved. In conclusion, we find that the bulk part of the flow was self-contained from a mass balance point of view and that that the overall amount of entrainment was limited.

Item Type:	Article
Date Type:	Publication
Status:	Published
Schools:	Earth and Environmental Sciences
Uncontrolled Keywords:	Mass-transport depositsSedimentologyFlow behaviourBasal shear zoneNankai Trough
Publisher:	Springer Verlag
ISSN:	1612-510X
Date of First Compliant Deposit:	19 October 2016
Date of Acceptance:	10 October 2016
Last Modified:	06 Dec 2024 13:45
URI:	https://orca.cardiff.ac.uk/id/eprint/95444

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