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Zisin (Journal of the Seismological Society of Japan 2nd ser )
Unsteady mantle convection is studied as a continuation of the previous paper (Part 1). Thermal interactions between the crust and the upper mantle are our main interests. Numerical calculations are performed until a reversal of the initial temperature distribution is realized. Variations in isotherm, speed, stress and heat flow through the Moho are obtained. The speed increases exponentially and reaches the order of 1 cm/year. The stage of the maximum stress comes 3-4x107 years earlier thandoi:10.4294/zisin1948.17.3_148 fatcat:vjknfcwuznhrrb46xb3dckv76m