| 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 |
| Genre: | Article |
| ProdID: | 70017106 |
| Citation Author: | Twichell, D. C.; Schwab, W. C.; Nelson, C. H.; Kenyon, N. H.; Lee, H. J. |
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| Citation End Page: | 692 |
| Citation Issue: | 8 |
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| Citation Language: | English |
| Citation Larger Work Title: | Geology |
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| Citation Number Of Pages: | 4 |
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| Citation Search Results Text: | Characteristics of a sandy depositional lobe on the outerMississippi Fan from Sea MARC 1A sidescan sonar images; 1992; Article; Journal; Geology; Twichell, D. C.; Schwab, W. C.; Nelson, C. H.; Kenyon, N. H.; Lee, H. J. |
| Citation Start Page: | 689 |
| Citation Volume: | 20 |
| Citation Year: | 1992 |
| Type: | citation/reference |
| Text: | Characteristics of a sandy depositional lobe on the outerMississippi Fan from Sea MARC 1A sidescan sonar images; 1992; Article; Journal; Geology; Twichell, D. C.; Schwab, W. C.; Nelson, C. H.; Kenyon, N. H.; Lee, H. J. |
| URL (THUMBNAIL): | http://pubs.er.usgs.gov/thumbnails/outside_thumb.jpg |
| Date Other: | Wed, 1 Jan 1992 00:00 -0600 |
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