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Asymmetric Continuum: Basic Motions and Equations

  • Roman Teisseyre
  • Maria Teisseyre-Jeleńska
Chapter
Part of the GeoPlanet: Earth and Planetary Sciences book series (GEPS)

Introduction

For axial, shear and rotational strains, we present the basic motion equations, which follow directly from the derivatives of the classic Newton formula; these motion equations can be quite independent; their reference displacements can be quite different. However, for the waves emitted from a common source (e.g., an earthquake focus) some of these motions might be correlated or phase shifted; these interaction fields explain the wave propagation due the rotation strain and shear strain mutual release-rebound processes. For a solid continuum we introduce the molecular transport motion as nuclei of a possible real transport inside a fracture domain. We consider also the important experimental data related to the appearances of the \( E_{\varphi \varphi } \)

Keywords

Molecular Transport Deviatoric Strain Double Couple Stress Moment Reference Displacement 
These keywords were added by machine and not by the authors. This process is experimental and the keywords may be updated as the learning algorithm improves.

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Copyright information

© Springer-Verlag Berlin Heidelberg 2014

Authors and Affiliations

  1. 1.Institute of GeophysicsPolish Academy of SciencesWarsawPoland

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