The model of whole mantle convection with formation of a long living reservoir feeding the mid-ocean ridge


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This paper shows the results of numerical experiments that reproduce the main global structures in the mantle. In particular, it is shown how, under whole mantle convection, a subducting plate produces circulation currents feeding the mid-ocean ridge.

作者简介

M. Evseev

Institute of Physics of the Earth

Email: trub@ifz.ru
俄罗斯联邦, Moscow, 123810

V. Trubitsyn

Institute of Physics of the Earth; Institute of the Theory of Earthquake Prediction and Mathematical Geophysics

编辑信件的主要联系方式.
Email: trub@ifz.ru
俄罗斯联邦, Moscow, 123810; Moscow, 113556

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