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Normark, William R. et al. (2002): Variability in form and growth of sediment waves on turbidite channel levees
Leg/Site/Hole:
Related Expeditions:
Identifier:
ID:
2003-018319
Type:
georefid
Creator:
Name:
Normark, William R.
Affiliation:
U. S. Geological Survey, Menlo Park, CA, United States
Role:
author
Name:
Piper, David J. W.
Affiliation:
Geological Survey of Canada (Atlantic), Canada
Role:
author
Name:
Posamentier, Henry
Affiliation:
Anadarko Canada Corporation, Canada
Role:
author
Name:
Pirmez, Carlos
Affiliation:
Shell International Exploration and Production, United States
Role:
author
Name:
Migeon, Sebastien
Affiliation:
Role:
author
Identification:
Title:
Variability in form and growth of sediment waves on turbidite channel levees
Year:
2002
Source:
In: Wynn, Russell B. (editor), Stow, Dorrik A. V. (editor), Recognition and interpretation of deep-water sediment waves; implications for palaeoceanography, hydrocarbon exploration and flow process interpretation
Publisher:
Elsevier, Amsterdam, Netherlands
Volume:
192
Issue:
1-3
Pages:
23-58
Abstract:
Language:
English
Genre:
Serial
Rights:
URL:
Coverage:
Geographic coordinates:
North:49.0000
West:-92.1500
East: -44.0000
South:3.0000
Keywords:
Oceanography; Amazon Fan; Atlantic Ocean; bathymetry; bedding; bedding plane irregularities; bottom features; channels; cores; currents; deep-sea sedimentation; deep-water environment; East Pacific; fine-grained materials; geophysical methods; geophysical profiles; geophysical surveys; Great Lakes; high-resolution methods; Huenema Fan; lacustrine sedimentation; Lake Superior; laminations; levees; marine sedimentation; marine sediments; Monterey Fan; morphometry; North America; North Atlantic; North Pacific; Northeast Pacific; Ocean Drilling Program; ocean floors; Pacific Ocean; petroleum; planar bedding structures; planforms; reflection methods; Reserve Fan; reservoir rocks; sand waves; sedimentary structures; sedimentation; sediments; seismic methods; seismic profiles; submarine fans; surveys; textures; turbidite; turbidity currents;
.
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