Facies distribution and textural variation in Faro Drift contourites: Velocity fluctuation and drift growth
- 1 June 1986
- journal article
- Published by Elsevier in Marine Geology
- Vol. 72 (1-2) , 71-100
- https://doi.org/10.1016/0025-3227(86)90100-3
Abstract
No abstract availableKeywords
This publication has 31 references indexed in Scilit:
- The High-Velocity Core of the Western Boundary Undercurrent at the Base of the U.S. Continental RiseScience, 1982
- Global paleoceanography and its deep water linkage to the Antarctic glaciationEarth-Science Reviews, 1980
- Distinguishing between fine‐grained turbidites and contourites on the Nova Scotian deep water marginSedimentology, 1979
- Paleocurrent Indicators in Deep-Sea SedimentScience, 1979
- The deep waters of the western North Atlantic during the past 24,000 years, and the re-initiation of the Western Boundary UndercurrentMarine Micropaleontology, 1979
- Paleoclimatology and paleo-oceanography of the Norwegian and Greenland Seas: The last 450,000 yearsMarine Micropaleontology, 1977
- Was there a late-Würm Arctic Ice Sheet?Nature, 1977
- Increased Transport of Antarctic Bottom Water in the Vema Channel During the Last Ice AgeScience, 1976
- No current reversal at 10,000 B.P. in the Strait of GibraltarMarine Geology, 1973
- Insolation changes, ice volumes, and the O18 record in deep‐sea coresReviews of Geophysics, 1970