Architecture of a coarse-grained channel-levee system

the Rosario Formation, Baja California, Mexico

Ian A. Kane, Mason L. Dykstra, Benjamin Charles Kneller, Sacha Tremblay, William D. McCaffrey

Research output: Contribution to journalArticle

53 Citations (Scopus)

Abstract

Seafloor images of coarse-grained submarine channel-levee systems commonly reveal complex braid-plain patterns of low-amplitude bedforms and zones of apparent bypass; however, mechanisms of channel evolution and the resultant channel-fill architecture are poorly understood. At Playa Esqueleto the lateral relationships between various elements of a deep-marine slope channel system are well-exposed. Specifically, the transition from gravel-dominated axial thalwegs to laterally persistent marginal sandstones and isolated gravel-filled scours is revealed. Marginal sandstones pass into a monotonous thin-bedded succession which built to form relatively low-relief levees bounding the channel belt; in turn, the levees onlap the canyon walls. Three orders of confinement were important during the evolution of the channel system: (i) first-order confinement was provided by the erosional canyon which confined the entire system; (ii) confined levees built of turbidite sandstones and mudstones formed the second-order confinement, and it is demonstrated that these built from overspill at thalweg margins; and (iii) third-order confinement describes the erosional confinement of coarse-grained thalwegs and scours. Finer-grained sediment was transported in suspension and largely was unaffected by topography at the scale of individual thalwegs. Facies and clast analyses of conglomerate overlying channel-marginal scours reveal that they were deposited by composite gravity flows, which were non-cohesive, grain-dominant debris flows with more fluidal cores. These flows were capable of basal erosion but were strongly depositional; frictional freezing at flow margins built gravel levees, while the core maintained a more fluidal transport regime. The resultant architecture consists of matrix-rich, poorly sorted levees bounding better-sorted, traction-dominated cores. The planform geometry is interpreted to have consisted of a low-sinuosity gravel braid-plain built by accretion around mid-channel and bank-attached bars. This part of the system may be analogous to fluvial systems; however, the finer-grained sediment load formed thick suspension clouds, probably several orders of magnitude thicker than the relief of braid-plain topography and therefore controlled by the levees and canyon wall confinement.

Original languageEnglish
Pages (from-to)2207-2234
Number of pages28
JournalSedimentology
Volume56
Issue number7
Early online date22 Jun 2009
DOIs
Publication statusPublished - Dec 2009

Keywords

  • Architecture
  • channel-levee
  • conglomerate
  • deep marine
  • submarine channel
  • density turbidity currents
  • water escape structures
  • deep-water
  • debris-flow
  • accretion deposits
  • sinuous channels
  • Southern Chile
  • facies models
  • fan-channel

Cite this

Kane, I. A., Dykstra, M. L., Kneller, B. C., Tremblay, S., & McCaffrey, W. D. (2009). Architecture of a coarse-grained channel-levee system: the Rosario Formation, Baja California, Mexico. Sedimentology, 56(7), 2207-2234. https://doi.org/10.1111/j.1365-3091.2009.01077.x

Architecture of a coarse-grained channel-levee system : the Rosario Formation, Baja California, Mexico. / Kane, Ian A.; Dykstra, Mason L.; Kneller, Benjamin Charles; Tremblay, Sacha; McCaffrey, William D.

In: Sedimentology, Vol. 56, No. 7, 12.2009, p. 2207-2234.

Research output: Contribution to journalArticle

Kane, Ian A. ; Dykstra, Mason L. ; Kneller, Benjamin Charles ; Tremblay, Sacha ; McCaffrey, William D. / Architecture of a coarse-grained channel-levee system : the Rosario Formation, Baja California, Mexico. In: Sedimentology. 2009 ; Vol. 56, No. 7. pp. 2207-2234.
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AU - McCaffrey, William D.

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AB - Seafloor images of coarse-grained submarine channel-levee systems commonly reveal complex braid-plain patterns of low-amplitude bedforms and zones of apparent bypass; however, mechanisms of channel evolution and the resultant channel-fill architecture are poorly understood. At Playa Esqueleto the lateral relationships between various elements of a deep-marine slope channel system are well-exposed. Specifically, the transition from gravel-dominated axial thalwegs to laterally persistent marginal sandstones and isolated gravel-filled scours is revealed. Marginal sandstones pass into a monotonous thin-bedded succession which built to form relatively low-relief levees bounding the channel belt; in turn, the levees onlap the canyon walls. Three orders of confinement were important during the evolution of the channel system: (i) first-order confinement was provided by the erosional canyon which confined the entire system; (ii) confined levees built of turbidite sandstones and mudstones formed the second-order confinement, and it is demonstrated that these built from overspill at thalweg margins; and (iii) third-order confinement describes the erosional confinement of coarse-grained thalwegs and scours. Finer-grained sediment was transported in suspension and largely was unaffected by topography at the scale of individual thalwegs. Facies and clast analyses of conglomerate overlying channel-marginal scours reveal that they were deposited by composite gravity flows, which were non-cohesive, grain-dominant debris flows with more fluidal cores. These flows were capable of basal erosion but were strongly depositional; frictional freezing at flow margins built gravel levees, while the core maintained a more fluidal transport regime. The resultant architecture consists of matrix-rich, poorly sorted levees bounding better-sorted, traction-dominated cores. The planform geometry is interpreted to have consisted of a low-sinuosity gravel braid-plain built by accretion around mid-channel and bank-attached bars. This part of the system may be analogous to fluvial systems; however, the finer-grained sediment load formed thick suspension clouds, probably several orders of magnitude thicker than the relief of braid-plain topography and therefore controlled by the levees and canyon wall confinement.

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KW - channel-levee

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KW - submarine channel

KW - density turbidity currents

KW - water escape structures

KW - deep-water

KW - debris-flow

KW - accretion deposits

KW - sinuous channels

KW - Southern Chile

KW - facies models

KW - fan-channel

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