Architecture and morphodynamics of subcritical sediment waves in an ancient channel-lobe transition zone
Author:
Affiliation:
1. Stratigraphy Group; School of Earth and Environment; University of Leeds; Leeds LS2 9JT UK
2. School of Earth, Ocean and Ecological Sciences; University of Liverpool; Liverpool L69 3GP UK
Funder
Anadarko
Bayerngas Norge
BG Group
BHP Billiton
BP and Chevron
DONG Energy
Premier Oil
Engie
Maersk Oil
Marathon Oil
Petrobras
Shell
Statoil
Total
VNG Norge
Woodside
Publisher
Wiley
Subject
Stratigraphy,Geology
Link
http://onlinelibrary.wiley.com/wol1/doi/10.1111/sed.12468/fullpdf
Reference122 articles.
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2. A classification of climbing-ripple cross-lamination;Allen;J. Geol. Soc. London,1973
3. Parallel lamination developed from upper-stage plane beds: a model based on the larger coherent structures of the turbulent boundary layer;Allen;Sed. Geol.,1984
4. Postavulsion channel evolution: Niger Delta continental slope;Armitage;AAPG Bull.,2012
5. Washed-out ripples: their equilibrium dimensions, migration rate, and relation to suspended-sediment concentration in very fine sand;Baas;J. Sediment. Res.,1995
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