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Characteristics of a sandy depositional lobe on the outerMississippi Fan from Sea MARC 1A sidescan sonar images

Geology
By: , and 

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Abstract

Shows that channelized rather than unconfined transport was the dominant transport mechanism for coarse-grained sediment during the formation of this part of the deep-sea fan. The dendritic distributary pattern and the high order of splaying of the channels, only one of which appears to have been active at a time, suggest that coarse- grained deposits on this fan are laterally discontinuous. -from Authors
Publication type Article
Publication Subtype Journal Article
Title Characteristics of a sandy depositional lobe on the outerMississippi Fan from Sea MARC 1A sidescan sonar images
Series title Geology
Volume 20
Issue 8
Year Published 1992
Language English
Larger Work Type Article
Larger Work Subtype Journal Article
Larger Work Title Geology
First page 689
Last page 692
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