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Shaping of the Continental Rise by Deep Geostrophic Contour Currents

Science22 Apr 1966Vol 152, Issue 3721pp. 502-508DOI: 10.1126/science.152.3721.502

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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Published In

Science
Volume 152 | Issue 3721
22 April 1966

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Published in print: 22 April 1966

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Bruce C. Heezen
Lamont Geological Observatory of Columbia University, Palisades, New York 10964
Charles D. Hollister
Lamont Geological Observatory of Columbia University, Palisades, New York 10964
William F. Ruddiman
Lamont Geological Observatory of Columbia University, Palisades, New York 10964

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