Skip to main content

Research Repository

Advanced Search

Pulse propagation in turbidity currents

Ho, Viet Luan; Dorrell, Robert M.; Keevil, Gareth M.; Burns, Alan D.; McCaffrey, William D.

Authors

Viet Luan Ho

Gareth M. Keevil

Alan D. Burns

William D. McCaffrey



Contributors

Jaco Baas
Editor

Abstract

© 2017 The Authors. Sedimentology © 2017 International Association of Sedimentologists Submarine turbidity currents are a key mechanism in the transportation of clastic sediments to deep seas. Such currents may initiate with a complex longitudinal flow structure comprising flow pulses (for example, by being sourced from retrogressive sea floor slope failures) or acquire such structure during run-out (for example, following flow combination downstream of confluences). A key question is how far along channel pathway complex flow structure is preserved within turbidity currents as they run out and thus if flow initiation mechanism and proximity to source may be inferred from the vertical structure of their deposits. To address this question, physical modelling of saline flows has been conducted to investigate the dynamics of single-pulsed versus multi-pulsed density driven currents. The data suggest that, under most circumstances, individual pulses within a multi-pulsed flow must merge. Therefore, initiation signatures will only be preserved in deposits upstream of the merging point and may be distorted approaching it; downstream of the merging point, all initiation signals will be lost. This new understanding of merging phenomenon within multi-pulsed gravity currents broadens our ability to interpret multi-pulsed turbidites.

Citation

Ho, V. L., Dorrell, R. M., Keevil, G. M., Burns, A. D., & McCaffrey, W. D. (2018). Pulse propagation in turbidity currents. Sedimentology, 65(2), 620-637. https://doi.org/10.1111/sed.12397

Acceptance Date Sep 1, 2017
Online Publication Date Jun 26, 2017
Publication Date Feb 1, 2018
Deposit Date Mar 21, 2018
Publicly Available Date Jun 27, 2018
Journal Sedimentology
Print ISSN 0037-0746
Publisher Wiley
Peer Reviewed Peer Reviewed
Volume 65
Issue 2
Pages 620-637
DOI https://doi.org/10.1111/sed.12397
Keywords Multi-pulsed turbidity currents; pulsed turbidites; seismo-turbidites; signal shredding; stacked turbidites; turbidity currents
Public URL https://hull-repository.worktribe.com/output/733474
Publisher URL https://onlinelibrary.wiley.com/doi/abs/10.1111/sed.12397
Related Public URLs http://eprints.whiterose.ac.uk/118146/
Contract Date Mar 21, 2018

Files

Article (1.3 Mb)
PDF

Copyright Statement
© 2017 The Authors. Sedimentology © 2017 International Association of Sedimentologists. This is the peer reviewed version of the following article: Ho, V. L., Dorrell, R. M., Keevil, G. M., Burns, A. D. and McCaffrey, W. D. (2017), Pulse propagation in turbidity currents. Sedimentology., which has been published in final form at https://doi.org/10.1111/sed.12397. This article may be used for non-commercial purposes in accordance with Wiley Terms and Conditions for Self-Archiving. Uploaded in accordance with the publisher's self-archiving policy.






You might also like



Downloadable Citations