The failure propagation of weakly stable sediment: A reason for the formation of high-velocity turbidity currents in submarine canyons
Author:
Publisher
Springer Science and Business Media LLC
Subject
Water Science and Technology,Oceanography
Link
https://link.springer.com/content/pdf/10.1007/s00343-022-1285-0.pdf
Reference41 articles.
1. Azpiroz-Zabala M, Cartigny M J B, Talling P J et al. 2017. Newly recognized turbidity current structure can explain prolonged flushing of submarine canyons. Science Advances, 3(10): e1700200, https://doi.org/10.1126/sciadv.1700200.
2. Bagnold R A. 1962. Auto-suspension of transported sediment; turbidity currents. Proceedings of the Royal Society A: Mathematical, Physical and Engineering Sciences, 265(1322): 315–319, https://doi.org/10.1098/rspa.1962.0012.
3. Carter L, Gavey R, Talling P J et al. 2014. Insights into submarine geohazards from breaks in subsea telecommunication cables. Oceanography, 27(2): 58–67, https://doi.org/10.5670/oceanog.2014.40.
4. Carter L, Milliman J D, Talling P J et al. 2012. Near-synchronous and delayed initiation of long run-out submarine sediment flows from a record-breaking river flood, offshore Taiwan. Geophysical Research Letters, 39(12): L12603, https://doi.org/10.1029/2012gl051172.
5. Cooper C, Wood J, Imran J et al. 2016. Designing for turbidity currents in the Congo Canyon. In: Offshore Technology Conference. OTC, Houston, TX. OTC-26919-MSp, https://doi.org/10.4043/26919-ms.
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