The lithospheric-ionospheric interaction and the complex of accompanying anomalous physical phenomena caused by critical geodeformations and electrification of rocks are considered as precursors of earthquakes based on the criticality theory. It is shown that scaling of dislocation changes in critical geodeformations, which can be represented as a transition to a turbulent state of coseismic rheological flows, is responsible for the anomalous properties of physical phenomena. The resulting instability of physical processes provides a high energy of anomalous phenomena, contributing to their detection as precursors of earthquakes. The work was supported by IKIR FEB RAS State Task (subject registration  124012300245-2).

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Lithospheric-Ionospheric Interaction and Its Accompanying Phenomena

  • Boris Shevtsov,
  • Olga Sheremetyeva

摘要

The lithospheric-ionospheric interaction and the complex of accompanying anomalous physical phenomena caused by critical geodeformations and electrification of rocks are considered as precursors of earthquakes based on the criticality theory. It is shown that scaling of dislocation changes in critical geodeformations, which can be represented as a transition to a turbulent state of coseismic rheological flows, is responsible for the anomalous properties of physical phenomena. The resulting instability of physical processes provides a high energy of anomalous phenomena, contributing to their detection as precursors of earthquakes. The work was supported by IKIR FEB RAS State Task (subject registration  124012300245-2).