Open Journal of Earthquake Research

Volume 11, Issue 1 (February 2022)

ISSN Print: 2169-9623   ISSN Online: 2169-9631

Google-based Impact Factor: 0.81  Citations  

Self-Excitation of the Earthquakes

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DOI: 10.4236/ojer.2022.111002    198 Downloads   983 Views  Citations
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ABSTRACT

Numerous correlations between magnetic and seismic events unambiguously indicate that the magnetic control of the earthquakes is a fundamental phenomenon. It proceeds from the remarkable physics of magneto-plasticity of solids, which implies acceleration of dislocations by microwaves. The motion of dislocations provides release of dangerous elastic energy of the earthquake focus and transforms elastic energy into the safe energy of plastic deformation. Magneto-plasticity seems to be the most important mechanism of the magnetic control because the piezoelectric effect as a suggested mechanism of magnetic control should be excluded (Chelidze et al.). Magnetic control certifies earthquake focus as a receiver of microwaves; on the other side, numerous observations exhibit emission of microwaves generated by earthquake focus, so that it can be considered as a permanent generator of microwaves. The idea of this paper is to offer a mechanism of self-excitation of the focus: self-triggering is suggested to be induced by microwaves generated by earthquake focus itself. The more intensive is the crack formation, the higher is the density of microwaves, which accelerate dislocations and intensify crack formation: it is a feedback breeding, avalanche-like process. Both functions of earthquake focus, to be simultaneously generator and receiver of microwaves, are integrated into the same space and time. It excludes such limitation of the magnetic control as the penetrability of the rocks for microwaves.

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Buchachenko, A. (2022) Self-Excitation of the Earthquakes. Open Journal of Earthquake Research, 11, 18-30. doi: 10.4236/ojer.2022.111002.

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