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Updated: Jul 12, 2026

Evolution of Staircase Structures in Diffusive Convection
Published on: September 5, 2018
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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