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Acoustic Architecture Of Glaciolacustrine Sediments Deformed During Zonal Stagnation Of The Laurentide Ice Sheet; Mazinaw Lake,.pdf

Acoustic-Architecture-of-Glaciolocustrine-Sediments-Deformed-During-Zonal-Stagnation-of-the-Laurentide-Ice-Sheet.pdf
Preview of Acoustic Architecture of Glaciolacustrine Sediments Deformed During Zonal Stagnation of the Laurentide Ice Sheet; Mazinaw Lake,
🔗 Source: marinemagnetics.com
📊 Size: 1.71 MB
📄 Pages: 19 pages
⬇️ Downloads: 71

Summary

Acoustic architecture of glaciolacustrine sediments deformed during zonal stagnation of the Laurentide Ice Sheet was studied at Mazinaw Lake, Ontario, Canada. The lake's sediment floor is pitted with steep-sided, enclosed depressions (kettle basins) formed by the melt of stagnant ice blocks and collapse of sediment. High-resolution seismic reflection, magnetic, and bathymetric surveys revealed large-scale normal faults, fractures, rotational failures, and incoherent chaotically bedded sediment. The deformation is likely a result of rapid melt of buried ice blocks, rather than neotectonic earthquake activity. The location and shape of buried ice masses were controlled by the graben-like form of the underlying bedrock surface.

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Acoustic architecture of glaciolacustrine sediments deformed during zonal stagnation of the Laurentide Ice Sheet was studied at Mazinaw Lake, Ontario, Canada.

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  • File Format: PDF
  • File Size: 1.71 MB
  • Pages: 19
  • Language: EN
  • Total Downloads: 71
  • Last Updated: 1 month ago

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