It follows from the basic principles of mechanics of deformable solids relating to the strength,
stability and propagation of elastic waves that the inner core of the Earth cannot exist in the …

It follows from the basic principles of mechanics of deformable solids relating to the strength,
stability and propagation of elastic waves that the Earth's inner core cannot exist in the form …

It is shown that the distribution of basic physico-mechanicalelastic properties and
parameters of the medium (such as elasticity moduli, density, pressure, etc.) in modern …

We studied the isotropic ball using data of Preliminary Reference Earth Model (PREM). It is
shown that such a ball should be either destructed or gone into a more stable equilibrium …

The study of behavior and values of deformations in the geological medium makes the
scientific basis of the methodology of synthesis of true values of parameters of its physico …

Strain occurs in solids within certain limits continuously. The state of elastic equilibrium is
stable within these limits. The change of elastic equilibrium state occurs in reaching strain …

ABSTRACT A theoretical method for determining variation intervals of strains is suggested
within which the conditions of reliable determination of values of elastic parameters of …

It follows from the basic principles of mechanics of deformable solids relating to the strength,
stability and propagation of elastic waves that the inner core of the Earth cannot exist in the …

The inner structure of the Earth's core and the distribution of its main parameters are well-
known and generally accepted. Pressure level reaches a value that is significantly greater …

Комплексная интерпретация разнообразных косвенных геофизических и
многочисленных лабораторно-экспериментальных данных показывает, что ядро …