Turbidity Currents With Equilibrium Basal Driving Layers: A Mechanism for Long Runout-Reference-Cited by-同舟云学术

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Turbidity Currents With Equilibrium Basal Driving Layers: A Mechanism for Long Runout

Published:2018-02-10 Issue:3 Volume:45 Page:1518-1526
ISSN:0094-8276
Container-title:Geophysical Research Letters
language:en
Short-container-title:Geophys. Res. Lett.

Author:

Luchi R.¹^ORCID,Balachandar S.²,Seminara G.³,Parker G.¹⁴^ORCID

Affiliation:

1. Department of Civil and Environmental EngineeringUniversity of Illinois at Urbana‐Champaign Urbana IL USA

2. Department of Mechanical and Aerospace EngineeringUniversity of Florida Gainesville FL USA

3. Department of Civil, Chemical and Environmental EngineeringUniversity of Genoa Genoa Italy

4. Department of GeologyUniversity of Illinois at Urbana‐Champaign Urbana IL USA

Publisher

American Geophysical Union (AGU)

Subject

General Earth and Planetary Sciences,Geophysics

Link

https://onlinelibrary.wiley.com/doi/pdf/10.1002/2017GL075608

Reference42 articles.

1. Newly recognized turbidity current structure can explain prolonged flushing of submarine canyons

2. Sedimentary Architecture in Meanders of a Submarine Channel: Detailed Study of the Present Congo Turbidite Channel (Zaiango Project)

3. Quaternary Depositional Systems in Northern Lake Baikal, Siberia

4. Dynamic Reynolds stress modeling of turbidity currents

5. Turbidity current with a roof: Direct numerical simulation of self-stratified turbulent channel flow driven by suspended sediment

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