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The spatial and temporal distribution of grain-size breaks in turbidites

The spatial and temporal distribution of grain-size breaks in turbidites
The spatial and temporal distribution of grain-size breaks in turbidites
Grain-size breaks are surfaces where abrupt changes in grain size occur vertically within deposits. Grain-size breaks are common features in turbidites around the world, including ancient and modern systems. Despite their widespread occurrence, grain-size breaks have been regarded as exceptional, and not included within idealized models of turbidity current deposition. This study uses ca 100 shallow sediment cores, from the Moroccan Turbidite System, to map out five turbidite beds for distances in excess of 2000 km. The vertical and spatial distributions of grain-size breaks within these beds are examined. Five different types of grain-size break are found: Type I – in proximal areas between coarse sand and finer grained structureless sand; Type II – in proximal areas between inversely graded sand overlain by finer sand; Type III – in proximal areas between sand overlain by ripple cross-laminated finer sand; Type IV – throughout the system between clean sand and mud; and Type V – in distal areas between mud-rich (debrite) sand and mud. This article interprets Types I and V as being generated by sharp vertical concentration boundaries, controlled by sediment and clay concentrations within the flows, whilst Types II and III are interpreted as products of spatial/temporal fluctuations in flow capacity. Type IV are interpreted as the product of fluid mud layers, which hinder the settling of non-cohesive grains and bypasses them down slope. Decelerating suspensions with sufficient clay will always form cohesive layers near to bed, promoting the generation of Type IV grain-size breaks. This may explain why Type IV grain-size breaks are widespread in all five turbidites examined and are commonplace within turbidite sequences studied elsewhere. Therefore, Type IV grain-size breaks should be understood as the norm, not the exception, and regarded as a typical feature within turbidite beds.
Bed correlation, fluid mud, grain-size break, Moroccan Turbidite System, turbidite
0037-0746
1120-1156
Stevenson, Christopher J.
4dd8706f-1d26-437c-95d0-6e131a5ec078
Talling, Peter J.
1cbac5ec-a9f8-4868-94fe-6203f30b47cf
Masson, Douglas G.
edd44c8b-38ca-45fb-8d0d-ac8365748a45
Sumner, Esther J.
dbba4b92-89cc-45d9-888e-d0e87e5c10ac
Frenz, Michael
8c9cae60-8127-447e-91fb-94a442444f75
Wynn, Russell B.
72ccd765-9240-45f8-9951-4552b497475a
Stevenson, Christopher J.
4dd8706f-1d26-437c-95d0-6e131a5ec078
Talling, Peter J.
1cbac5ec-a9f8-4868-94fe-6203f30b47cf
Masson, Douglas G.
edd44c8b-38ca-45fb-8d0d-ac8365748a45
Sumner, Esther J.
dbba4b92-89cc-45d9-888e-d0e87e5c10ac
Frenz, Michael
8c9cae60-8127-447e-91fb-94a442444f75
Wynn, Russell B.
72ccd765-9240-45f8-9951-4552b497475a

Stevenson, Christopher J., Talling, Peter J., Masson, Douglas G., Sumner, Esther J., Frenz, Michael and Wynn, Russell B. (2014) The spatial and temporal distribution of grain-size breaks in turbidites. Sedimentology, 61 (4), 1120-1156. (doi:10.1111/sed.12091).

Record type: Article

Abstract

Grain-size breaks are surfaces where abrupt changes in grain size occur vertically within deposits. Grain-size breaks are common features in turbidites around the world, including ancient and modern systems. Despite their widespread occurrence, grain-size breaks have been regarded as exceptional, and not included within idealized models of turbidity current deposition. This study uses ca 100 shallow sediment cores, from the Moroccan Turbidite System, to map out five turbidite beds for distances in excess of 2000 km. The vertical and spatial distributions of grain-size breaks within these beds are examined. Five different types of grain-size break are found: Type I – in proximal areas between coarse sand and finer grained structureless sand; Type II – in proximal areas between inversely graded sand overlain by finer sand; Type III – in proximal areas between sand overlain by ripple cross-laminated finer sand; Type IV – throughout the system between clean sand and mud; and Type V – in distal areas between mud-rich (debrite) sand and mud. This article interprets Types I and V as being generated by sharp vertical concentration boundaries, controlled by sediment and clay concentrations within the flows, whilst Types II and III are interpreted as products of spatial/temporal fluctuations in flow capacity. Type IV are interpreted as the product of fluid mud layers, which hinder the settling of non-cohesive grains and bypasses them down slope. Decelerating suspensions with sufficient clay will always form cohesive layers near to bed, promoting the generation of Type IV grain-size breaks. This may explain why Type IV grain-size breaks are widespread in all five turbidites examined and are commonplace within turbidite sequences studied elsewhere. Therefore, Type IV grain-size breaks should be understood as the norm, not the exception, and regarded as a typical feature within turbidite beds.

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More information

e-pub ahead of print date: 21 March 2014
Published date: June 2014
Keywords: Bed correlation, fluid mud, grain-size break, Moroccan Turbidite System, turbidite
Organisations: Geology & Geophysics, Marine Geoscience

Identifiers

Local EPrints ID: 363423
URI: http://eprints.soton.ac.uk/id/eprint/363423
ISSN: 0037-0746
PURE UUID: 45e2a044-8630-4761-9d92-23cf923b845b

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Date deposited: 24 Mar 2014 15:02
Last modified: 14 Mar 2024 16:24

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Contributors

Author: Christopher J. Stevenson
Author: Peter J. Talling
Author: Douglas G. Masson
Author: Michael Frenz
Author: Russell B. Wynn

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