Edge-driven convection
- Creators
- King, Scott D.
- Anderson, Don L.
Abstract
We consider a series of simple calculations with a step-function change in thickness of the lithosphere and imposed, far-field boundary conditions to illustrate the influence of the lithosphere on mantle flow. We consider the effect of aspect ratio and far-field boundary conditions on the small-scale flow driven by a discontinuity in the thickness of the lithosphere. In an isothermal mantle, with no other outside influences, the basic small-scale flow aligns with the lithosphere such that there is a downwelling at the lithospheric discontinuity (edge-driven flow); however, the pattern of the small-scale flow is strongly dependent on the large-scale thermal structure of a much broader area of the upper mantle. Long-wavelength temperature anomalies in the upper mantle can overwhelm edge-driven flow on a short timescale; however, convective motions work to homogenize these anomalies on the order of 100 million years while cratonic roots can remain stable for longer time periods. A systematic study of the effect of the boundary conditions and aspect ratio of the domain shows that small-scale, and large-scale flows are driven by the lithosphere. Edge-driven flow produces velocities on the order of 20 mm/yr. This is comparable to calculations by others and we can expect an increase in this rate as the mantle viscosity is decreased.
Additional Information
© 1998 Elsevier Science B.V. Received 15 January 1998; revised version received 21 April 1998; accepted 28 April 1998.Additional details
- Eprint ID
- 34809
- DOI
- 10.1016/S0012-821X(98)00089-2
- Resolver ID
- CaltechAUTHORS:20121010-083642138
- Created
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2012-10-10Created from EPrint's datestamp field
- Updated
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2021-11-09Created from EPrint's last_modified field