GEOSCAN, résultats de la recherche


TitreHow are subaqueous sediment density flows triggered, what is their internal structure and how does it evolve? Direct observations from monitoring of active flows
AuteurTalling, P J; Paull, C K; Piper, D J W
SourceEarth-Science Reviews vol. 125, 2013 p. 244-287, (Accès ouvert)
Séries alt.Secteur des sciences de la Terre, Contribution externe 20110291
ÉditeurElsevier BV
Documentpublication en série
Mediapapier; en ligne; numérique
ProvinceRégion extracotière de l'est; Région extracotière de l'ouest; Nunavut; Colombie-Britannique
Lat/Long OENS-58.0000 -50.0000 45.0000 36.0000
Lat/Long OENS-57.5000 -54.0000 45.0000 43.1667
Lat/Long OENS-57.0000 -50.0000 43.0000 35.0000
Lat/Long OENS 7.0000 9.0000 44.0000 42.5000
Lat/Long OENS119.0000 121.0000 22.0000 19.0000
Lat/Long OENS-121.8417 -121.8417 36.8042 36.7917
Lat/Long OENS 8.6667 8.6667 -5.6667 -5.9167
Lat/Long OENS-124.7500 -124.7500 50.9167 50.5000
Lat/Long OENS-123.5000 -123.0000 49.2500 48.7500
Lat/Long OENS-138.5000 -138.0000 61.2500 61.0000
Sujetsturbidites; courants de turbidite; sédimentation turbiditique; sedimentation; courants de densité; cônes sous-marins; glissements de pentes; canyons sous-marins; systèmes fluviaux; résidus; inondations; géologie marine; sédimentologie
ProgrammeGéoscience en mer, La géoscience pour les développements extracôtiers de la côte est
Résumé(disponible en anglais seulement)
Subaqueous sediment density flows are one of the volumetrically most important processes formoving sediment across our planet, and formthe largest sediment accumulations on Earth (submarine fans). They are also arguably the most sparely monitored major sediment transport processes on our planet. Significant advances have been made in documenting their timing and triggers, especiallywithin submarine canyons and delta-fronts, and freshwater lakes and reservoirs, but the sediment concentration of flows that run out beyond the continental slope has never beenmeasured directly. This limited amount ofmonitoring data contrasts sharply with other major types of sediment flow, such as river systems, and ensure that understanding submarine sediment density flows remains a major challenge for Earth science. The available monitoring data define a series of flow types whose character and deposits differ significantly. Large (N100 km3) failures on the continental slope can generate fast-moving (up to 19 m/s) flows that reach the deep ocean, and deposit thick layers of sand across submarine fans. Even small volume (0.008 km3) canyon head failures can sometimes generate channelised flows that travel at N5 m/s for several hundred kilometres. A single event off SE Taiwan shows that river floods can generate powerful flows that reach the deep ocean, in this case triggered by failure of recently deposited sediment in the canyon head. Direct monitoring evidence of powerful oceanic flows produced by plunging hyperpycnal
flood water is lacking, although this process has produced shorter and weaker oceanic flows. Numerous flows can occur each year on river-fed delta fronts, where they can generate up-slope migrating crescentic bedforms. These flows tend to occur during the flood season, but are not necessarily associated with individual flood discharge peaks, suggesting that they are often triggered by delta-front slope failures. Powerful flows occur several times each year in canyons fed by sand from the shelf, associated with strong wave action. These flows can
also generate up-slope migrating crescentic bedforms that most likely originate due to retrogressive breaching associated with a dense near-bed layer of sediment. Expanded dilute flows that are supercritical and fully turbulent are also triggered by wave action in canyons. Sediment density flows in lakes and reservoirs generated by plunging river flood water have been monitored in much greater detail. They are typically very dilute
(b0.01 vol.% sediment) and travel at b50 cm/s, and are prone to generating interflows within the density stratified freshwater. A key objective for future work is to develop measurement techniques for seeing through overlying dilute clouds of sediment, to determine whether dense near-bed layers are present. There is also a need to combine monitoring of flows with detailed analyses of flow deposits, in order to understand how flows are recorded in the rock record. Finally, a source-to-sink approach is needed because the character of submarine flows can change significantly along their flow path.