Abstract
A model for convection in the upper mantle of the Earth comprising two flows, one of percolating melt fluid (which need be no more than a small volume fraction in the intergranular channels of coherent solid matter), the other a solid plastic flow, avoids some paradoxical features of other models for mantle convection. This model leads to a reasonably consistent account of the processes of continental drift.
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References
Jacobs, J. A., Russell, R. D., and Wilson, J. T., Physics and Geology (McGraw-Hill, New York, 1959).
Blackett, P. M. S., Bullard, E., and Runcorn, S. K., A Symposium on Continental Drift, Phil. Trans. Roy. Soc., A, 258, 1 (1965).
Upper Mantle Meeting, University of Newcastle, 1966, Geophys. J. Roy. Astro. Soc., 14, Nos. 1–4 (1967); also published as Non-Elastic Processes in the Earth's Mantle (edit. by Tozer, D. C.) (Blackwell, Oxford, 1968).
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FRANK, F. Two-component Flow Model for Convection in the Earth's Upper Mantle. Nature 220, 350–352 (1968). https://doi.org/10.1038/220350a0
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DOI: https://doi.org/10.1038/220350a0
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