Deformations, corresponding to processes of consolidation, deconsolidation and phase transitions in internal structures of the Earth
© H.H. Guliyev
Questions of distribution of medium depending on changes of deformation have been studied involving various elastic potentials using
non-classical linearized approach within the limits of theory of small and large initial deformations and it has been shown that this
dependence for various geological media is instable. Given processes contribute to emergence of structures of formation
deconsolidation zones. In presence of different kinds of inclusions, free and contacted surfaces and cavities the process of
deformation occurs differently than assumed in experiments. Comparing the received theoretical results with results of known
experimental studies, it has been shown that the processes of loss of stability of elastic state of equilibrium on geometric shape
change and on "internal" instability precedes the processes of phase transitions of various mineral systems.
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