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Stress-strain state in an elastic medium containing an inclusion of a new phase
No full textThe problem of elastic equilibrium of an isotropic solid phase with a melt is examined in connection with a study of problems of magma generation and volcanic earthquakes. For the case of a spherical inclusion and zero pressure at infinity the stress-strain state is calculated to terms of the second order of smallness (with respect to the relative difference of densities of the phases)
