Asymmetric convection in the upper mantle
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Abstract
The New Global Tectonics admits convection in the upper mande as one of the possible driving forces. An experimental model which permits the study of convection in a fluid with internal homogeneous heat generation has been constructed. The development of asymmetric convection patterns suggests some in-teresting geophysical interpretations.
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De la Cruz Reyna, S. (1970). Asymmetric convection in the upper mantle. Geofisica Internacional, 10(2), 49–56. https://doi.org/10.22201/igeof.00167169p.1970.10.2.1166
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