New evidence for widespread mass transport on the Northeast Newfoundland Shelf revealed by Olex single-beam echo sounding |
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Authors: | John Shaw David J W Piper Thomas Skulski Michael J Lamplugh Andrew Craft André Roy |
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Institution: | (1) Geological Survey of Canada (Atlantic), P.O. Box 1006, Dartmouth, NS, B2Y 4A2, Canada;(2) Natural Resources Canada, 615 Booth Street, Ottawa, ON, K1A 0E9, Canada;(3) Canadian Hydrographic Service, Fisheries and Oceans Canada, P.O. Box 1006, Dartmouth, NS, B2Y 4A2, Canada;(4) Canadian Hydrographic Service, Fisheries and Oceans Canada, P.O. Box 5667, St. John’s, Newfoundland, A1C 5X1, Canada |
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Abstract: | Based on Olex single-beam sounder data, multibeam sonar surveys, and sparse seismic reflection profiles, we recognize a large
area of anomalous bathymetry on the Northeast Newfoundland Shelf as having formed as a result of mass-transport processes.
Transported masses include (1) an arcuate ridge of deformed material with an area of 430 km2, which has moved distances of ~20 km; (2) a 70-km2 mass of deformed material displaced 50 km along a nearly horizontal track flanked by 90-m-high berms. The movement of these
and other sediment bodies has created a 150-m-high headwall escarpment extending 110 km along the north flank of the Notre
Dame glacial trough. In addition, a 35-km2 block of undeformed material has moved 5 km to the southeast, away from the headwall, creating a gap of the same dimensions,
while a smaller block of material originating in this vicinity has been displaced 24 km in the opposite direction, creating
a 20-m-deep groove on the seafloor. There is evidence for mass transport and headwall formation elsewhere on the Northeast
Newfoundland Shelf. Analysis of seismic reflection data indicates that the transported material most likely consists of stacked
Quaternary till sheets that overlie Cenozoic, Mesozoic and older sedimentary rocks. Given the very low gradients involved,
glaciotectonism is the most likely process to account for transport and deformation of the large sediment masses. However,
some mass transport may have resulted from submarine sliding away from the headwalls that were created by the glacial transport. |
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