Erosion and Ponding of Thunder Horse Deep-Water Turbidites by Mass Transport Complexes in Mississippi Canyon Based on Image Log Sedimentology

Geometry and kinematics of Neogene allochthonous salt systems in the Mississippi Canyon, Atwater Valley, western Lloyd Ridge, and western DeSoto Canyon protraction areas, northern deep-water Gulf of Mexico

AAPG Bulletin ◽

10.1306/09011609186 ◽

2017 ◽

Vol 101 (07) ◽

pp. 1003-1034 ◽

Cited By ~ 5

Author(s):

Renaud Bouroullec ◽

Paul Weimer

Keyword(s):

Gulf Of Mexico ◽

Deep Water ◽

Mississippi Canyon ◽

Salt Systems ◽

Geometry And Kinematics

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MASS TRANSPORT IN VOCOIDAL THEORY

Coastal Engineering Proceedings ◽

10.9753/icce.v18.22 ◽

1982 ◽

Vol 1 (18) ◽

pp. 22

Author(s):

J.W. Gonsalves ◽

D.H. Swart

Keyword(s):

Free Surface ◽

Mass Transport ◽

Deep Water

The concept of mass transport is theoretically discussed within the framework provided by Vocoidal theory. The Lagrangian mass transport is divided into two parts; firstly treating the fluid as being inviscid and secondly, incorporating viscosity by means of the free surface and bottom boundaries. Eulerian mass transport is defined and is shown to correspond, in deep water, to the net flow predicted by Stokes and others.

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Mass Transport in Deep-Water Waves

Journal of Physical Oceanography ◽

10.1175/1520-0485(1978)008<1009:mtidww>2.0.co;2 ◽

1978 ◽

Vol 8 (6) ◽

pp. 1009-1015 ◽

Cited By ~ 19

Author(s):

Ole Secher Madsen

Keyword(s):

Mass Transport ◽

Deep Water ◽

Water Waves ◽

Deep Water Waves

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Reply [to “Discussion of paper by Ming-Shun Chang, ‘The mass transport in deep-water long-crested random gravity waves’”]

Journal of Geophysical Research Atmospheres ◽

10.1029/jc075i012p02213 ◽

1970 ◽

Vol 75 (12) ◽

pp. 2213-2213

Author(s):

Ming-Shun Chang

Keyword(s):

Mass Transport ◽

Gravity Waves ◽

Deep Water

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On mass transport in deep water waves

Pure and Applied Geophysics ◽

10.1007/bf02007111 ◽

1962 ◽

Vol 53 (1) ◽

pp. 65-76 ◽

Cited By ~ 3

Author(s):

J. N. Hunt ◽

S. K. A. Massoud

Keyword(s):

Mass Transport ◽

Deep Water ◽

Water Waves ◽

Deep Water Waves

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DFTopoSim: Modeling Topographically-Controlled Deposition of Subseismic Scale Sandstone Packages Within a Mass Transport Dominated Deep-Water Channel Belt

Mathematical Geosciences ◽

10.1007/s11004-013-9444-7 ◽

2013 ◽

Vol 45 (3) ◽

pp. 277-296 ◽

Cited By ~ 4

Author(s):

Lisa Stright ◽

Anne Bernhardt ◽

Alexandre Boucher

Keyword(s):

Mass Transport ◽

Deep Water ◽

Water Channel ◽

Channel Belt ◽

Controlled Deposition

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Regional structural setting and evolution of the Mississippi Canyon, Atwater Valley, western Lloyd Ridge, and western DeSoto Canyon protraction areas, northern deep-water Gulf of Mexico

AAPG Bulletin ◽

10.1306/09011609187 ◽

2017 ◽

Vol 101 (07) ◽

pp. 1035-1071 ◽

Cited By ~ 3

Author(s):

Renaud Bouroullec ◽

Paul Weimer ◽

Olivier Serrano

Keyword(s):

Gulf Of Mexico ◽

Deep Water ◽

Structural Setting ◽

Mississippi Canyon

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Mass transport in gravity waves

Mathematical Proceedings of the Cambridge Philosophical Society ◽

10.1017/s0305004100028140 ◽

1953 ◽

Vol 49 (1) ◽

pp. 145-150 ◽

Cited By ~ 11

Author(s):

F. Ursell

Keyword(s):

Solitary Wave ◽

Mass Transport ◽

Gravity Waves ◽

Deep Water ◽

Wave Motion ◽

Finite Depth ◽

Particle Displacement ◽

Slow Drift

ABSTRACTA proof is given of the existence of a slow drift associated with the passage of gravity waves over the surface of a frictionless fluid when the wave motion is irrotational. The drift is in the direction of propagation and is greatest near the surface, decreasing steadily towards the bottom, where it may be negative if the fluid is of finite depth. The particle displacement due to a solitary wave has similar properties. The proof confirms the approximate calculations of Stokes (6) and extends the proof of Rayleigh applicable only to deep water.

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