Shaping of the Continental Rise by Deep Geostrophic Contour Currents
Abstract
Geostrophic contour-following bottom currents involved in the deep thermohaline circulation of the world ocean appear to be the principal agents which control the shape of the continental rise and other sediment bodies.
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Science
Volume 152 | Issue 3721
22 April 1966
22 April 1966
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1966 by the American Association for the Advancement of Science.
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Published in print: 22 April 1966
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