Using sea-floor morphometrics to constrain stratigraphic models of sinuous submarine channel systems

2016 ◽  
Vol 77 ◽  
pp. 92-115 ◽  
Author(s):  
Aaron P. Reimchen ◽  
Stephen M. Hubbard ◽  
Lisa Stright ◽  
Brian W. Romans
Sedimentology ◽  
2014 ◽  
Vol 61 (4) ◽  
pp. 1031-1054 ◽  
Author(s):  
Jacob A. Covault ◽  
Svetlana Kostic ◽  
Charles K. Paull ◽  
Holly F. Ryan ◽  
Andrea Fildani

2019 ◽  
Vol 10 (1) ◽  
Author(s):  
F. Pohl ◽  
J. T. Eggenhuisen ◽  
M. Tilston ◽  
M. J. B. Cartigny

Abstract Particle-laden gravity flows, called turbidity currents, flow through river-like channels across the ocean floor. These submarine channels funnel sediment, nutrients, pollutants and organic carbon into ocean basins and can extend for over 1000’s of kilometers. Upon reaching the end of these channels, flows lose their confinement, decelerate, and deposit their sediment load; this is what we read in textbooks. However, sea floor observations have shown the opposite: turbidity currents tend to erode the seafloor upon losing confinement. Here we use a state-of-the-art scaling method to produce the first experimental turbidity currents that erode upon leaving a channel. The experiments reveal a novel flow mechanism, here called flow relaxation, that explains this erosion. Flow relaxation is rapid flow deformation resulting from the loss of confinement, which enhances basal shearing of the turbidity current and leads to scouring. This flow mechanism plays a key role in the propagation of submarine channel systems.


2021 ◽  
Author(s):  
Joris Eggenhuisen ◽  
Mike Tilston ◽  
Christopher Stevenson ◽  
Steve Hubbard ◽  
Matthieu Cartigny ◽  
...  

AAPG Bulletin ◽  
2012 ◽  
Vol 96 (10) ◽  
pp. 1813-1841 ◽  
Author(s):  
Jeremiah D. Moody ◽  
David R. Pyles ◽  
Julian Clark ◽  
Renaud Bouroullec

2015 ◽  
Vol 4 (1) ◽  
pp. 1142-1160 ◽  
Author(s):  
Prerna Ramesh ◽  
◽  
Dhananjai Kumar Pandey ◽  
Ravi Mishra ◽  
◽  
...  

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