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Genomes 4. Fourth edition
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Numerical models of thermally activated convective flow in Earth's mantle do not resemble active plate tectonics because of their inability to model successfully the process of subduction, other than by the inclusion of artificial weak zones. Here we show, using a boundary layer argument, how the "rigid lid" style of convection favored by thermoviscous fluids leads to lithospheric stresses whic...
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ژورنال
عنوان ژورنال: Journal of Applied Mechanics
سال: 1961
ISSN: 0021-8936,1528-9036
DOI: 10.1115/1.3641813