Conjugacy Problem for Stationary Heat Fields


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Abstract

An analytical solution for the stationary problem of thermal conjugation is obtained for the model of inhomogeneous layered media. The heat flux components for the crust and the mantle are separated. Recalculation of the mantle component of the flux down to the mantle top was performed, and the results were compared with the relief of deep structures.

About the authors

I. V. Ladovskiy

Institute of Geophysics, Ural Branch, Russian Academy
of Sciences

Email: pmart3@mail.ru
Russian Federation, Yekaterinburg

P. S. Martyshko

Institute of Geophysics, Ural Branch, Russian Academy
of Sciences

Author for correspondence.
Email: pmart3@mail.ru
Russian Federation, Yekaterinburg

D. D. Byzov

Institute of Geophysics, Ural Branch, Russian Academy
of Sciences

Email: pmart3@mail.ru
Russian Federation, Yekaterinburg

A. G. Tsidaev

Institute of Geophysics, Ural Branch, Russian Academy
of Sciences

Author for correspondence.
Email: pmart3@mail.ru
Russian Federation, Yekaterinburg

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