Powerful turbidity currents driven by dense basal layers

Seafloor sediment flows (turbidity currents) are among the volumetrically most important yet least documented sediment transport processes on Earth. A scarcity of direct observations means that basic characteristics, such as whether flows are entirely dilute or driven by a dense basal layer, remain...

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Detalles Bibliográficos
Autores principales: Paull, Charles K., Talling, Peter J., Maier, Katherine L., Parsons, Daniel, Xu, Jingping, Caress, David W., Gwiazda, Roberto, Lundsten, Eve M., Anderson, Krystle, Barry, James P., Chaffey, Mark, O’Reilly, Tom, Rosenberger, Kurt J., Gales, Jenny A., Kieft, Brian, McGann, Mary, Simmons, Steve M., McCann, Mike, Sumner, Esther J., Clare, Michael A., Cartigny, Matthieu J.
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Nature Publishing Group UK 2018
Materias:
Article
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC6173716/
https://www.ncbi.nlm.nih.gov/pubmed/30291228
http://dx.doi.org/10.1038/s41467-018-06254-6

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC6173716/
https://www.ncbi.nlm.nih.gov/pubmed/30291228
http://dx.doi.org/10.1038/s41467-018-06254-6

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