Sediment failure and sedimentary framework of the wilmington geotechnical corridor, U.S. atlantic continental margin
- 1 November 1981
- journal article
- Published by Elsevier in Sedimentary Geology
- Vol. 30 (3) , 213-234
- https://doi.org/10.1016/0037-0738(81)90041-5
Abstract
No abstract availableKeywords
This publication has 9 references indexed in Scilit:
- Mass movement of sediment on the continental slope and rise seaward of the Baltimore Canyon TroughMarine Geology, 1979
- Surficial slides and slumps on the continental slope and rise of South West Africa: A reconnaissance studyMarine Geology, 1979
- The “mud-line”: An erosion—Deposition boundary on the upper continental slopeMarine Geology, 1978
- Geotechnical properties of a submarine slide area on the U.S. continental slope northeast of Wilmington canyonMarine Geotechnology, 1977
- Distribution and morphology of large submarine sediment slides and slumps on Atlantic continental marginsMarine Geotechnology, 1977
- Large sand waves on the Atlantic Outer Continental Shelf around Wilmington Canyon, off Eastern United StatesMarine Geology, 1976
- Large submarine slide (olistostrome) associated with Sunda Arc subduction zone, northeast Indian OceanMarine Geology, 1976
- Morphology and Structure of Wilmington and Baltimore Submarine Canyons, Eastern United StatesThe Journal of Geology, 1970
- Interpretation of a Levee-like Ridge and Associated Features, Wilmington Submarine Canyon, Eastern United StatesGSA Bulletin, 1970