title: Paleocurrent indicators in deep-sea sediment.
abstract: The fabric and texture of deep-sea sediments have been used to detect periods of high-velocity bottom-water flow through the Vema Channel in the south-west Atlantic Ocean. In addition, the alignment of the long axis of magnetic grains has been used to indicate the direction of bottom-water flow.
authors.forename: B B
authors.initials: BB
authors.lastname: Ellwood
authors.forename: M T
authors.initials: MT
authors.lastname: Ledbetter