Abstract
The problem of the determination of thermomechanical conditions in the upper mantle under a moving lithospheric plate at a given shear stress does not have a unique solution. Given a fixed heat flux from the lower mantle, two types of motion are possible in the mantle: subcritical (slower and colder) and supercritical (faster and hotter). In this work, it is shown that, if these modes are rather close to each other (in the near-critical state of the mantle), transitions from one mode to another and backward are possible. The calculated period of a change in the mantle state amounts to ∼0.3 Myr for the Pacific plate. The oscillatory regime of the mantle state can manifest itself in the activity pulsations of hotspots located near fast separating mid-ocean ridges.
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Original Russian Text © S.V. Gavrilov, A.N. Boiko, 2008, published in Fizika Zemli, 2008, No. 1, pp. 44–49.
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Gavrilov, S.V., Boiko, A.N. On stochastic near-critical oscillations in the upper mantle. Izv., Phys. Solid Earth 44, 38–42 (2008). https://doi.org/10.1134/S1069351308010059
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DOI: https://doi.org/10.1134/S1069351308010059