Abstract
Crustal deformation processes occur with relative rapidity when short-term precursors appear at the final preparatory stage of a tectonic earthquake. This paper contains calculations of crustal bulk strain before an earthquake, based on the model of a rigid inclusion. The data give initial conditions for the problem of fluid percolation in a two-phase medium accompanied by electrokinetic effects. The solution provides a description of systems of currents arising in the vicinity of the source region. An analysis of this theoretical evidence yields information on the behaviour of short-term precursors in telluric currents and the geomagnetic field.
Original language | American English |
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Journal | Physics of the Earth and Planetary Interiors |
Volume | 57 |
DOIs | |
State | Published - Oct 1 1989 |
Disciplines
- Physical Sciences and Mathematics
- Physics