The magnetic fabric of surficial deep-sea sediments in the HEBBLE area (Nova Scotian continental rise)

This publication has 23 references indexed in Scilit:

• The High-Velocity Core of the Western Boundary Undercurrent at the Base of the U.S. Continental Rise
  Science, 1982
• Induced and remanent magnetic properties of marine sediments as indicators of depositional processes
  Marine Geology, 1980
• Tritium in the deep North Atlantic Ocean
  Nature, 1980
• Application of the anisotropy of magnetic susceptibility method as an indicator of bottom-water flow direction
  Marine Geology, 1980
• Sedimentary fabric: A tool to delineate a high-velocity zone within a deep western Indian Ocean bottom current
  Marine Geology, 1979
• Particle flocculation: One possible control on the magnetization of deep‐sea sediments
  Geophysical Research Letters, 1979
• Paleocurrent Indicators in Deep-Sea Sediment
  Science, 1979
• Antarctic bottom water fluctuations in the Vema Channel: Effects of velocity changes on particle alignment and size
  Earth and Planetary Science Letters, 1977
• Palaeocurrent determinations by magnetic fabric measurements on the Cambrian Rocks of St. Tudwal's Peninsula, North Wales
  Geological Journal, 1967
• Atlantic Deep-Sea Sediment Cores
  GSA Bulletin, 1961