Sediment mass-flow processes on a depositional lobe, outer Mississippi Fan

Journal of Sedimentary Research
By: , and 

Links

Abstract

SeaMARC 1A sidescan-sonar imagery and cores from the distal reaches of a depositional lobe on the Mississippi Fan show that channelized mass flow was the dominant mechanism for transport of silt and sand during the formation of this part of the fan. Sediments in these flows were rapidly deposited once outside of their confining channels. The mass flows most likely originated from slope failure at the head of the Mississippi Canyon or on the outer continental shelf and flowed approximately 500 km to the distal reaches of the fan, with debris flow being the dominant flow type.

Study Area

Additional publication details

Publication type Article
Publication Subtype Journal Article
Title Sediment mass-flow processes on a depositional lobe, outer Mississippi Fan
Series title Journal of Sedimentary Research
DOI 10.1306/D426843C-2B26-11D7-8648000102C1865D
Volume 66
Issue 5
Year Published 1996
Language English
Contributing office(s) Woods Hole Coastal and Marine Science Center
Description 12 p.
Larger Work Type Article
Larger Work Subtype Journal Article
Larger Work Title Journal of Sedimentary Research
First page 916
Last page 927
Country United States
State Mississippi
Other Geospatial Gulf of Mexico
Google Analytic Metrics Metrics page