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- Publisher
- Springer Journals
- Copyright
- 2012 Pleiades Publishing, Ltd.
- ISSN
- 1063-7745
- eISSN
- 1562-689X
- DOI
- 10.1134/s1063774512010105
- Publisher site
- See Article on Publisher Site
Abstract
Abstract Different geophysical data and conclusions of theoretical models, which can give information about the behavior of the solid and liquid cores of the Earth as well as about the existence of a transition layer as a temperature-hysteresis region at a relatively weak first-order phase transition, are compared. It is concluded that liquid inclusions inevitably exist in this region; these inclusions are involved (due to the complex convective processes occurring in the liquid core) in the transport of light materials from some areas of the solid-core surface. The porosity and permeability of the transition layer determine the seismic acoustic inhomogeneities in these areas, which contact the convective flows in the liquid core. In particular, this explains the well-known “east-west” effect. Obviously, the model of the crystalline core is not the only possible alternative for a model of a core with a metallic glasslike structure.
Journal
Crystallography Reports – Springer Journals
Published: May 1, 2012
Keywords: Crystallography and Scattering Methods