Abstract. This publication highlights theoretical work that could explain four different empirical observations indicating a direct relationship between magnetic fields and earthquakes, which would allow the description of a causal mechanism prior to and during the occurrence of earthquakes. These theoretical calculations seek to elucidate the role of the magnetic field in different aspects of solid earth dynamics, with an interest in the study and comprehension of the physics that could generate earthquakes accompanied by simultaneous magnetic signals within the lithosphere. The Motion of Charged Edge Dislocations (MCD) model and its correlation with the magnetic field have been used in order to include the generation of electric currents. The electric currents resulting from stress variation in the lithosphere helps us to analyze the lithosphere as a critical system, before and after the occurrence of earthquakes, by using the concept of earthquake entropy. Where it is found that the non-existence of seismic and magnetic precursors could be interpreted as a violation to the second law of thermodynamics. In addition, the Seismic Moment and the Moment Magnitude of some great earthquakes are quite accurately calculated using the co-seismic magnetic field. The distance-dependent co-seismic magnetic field has been theorized for some of the largest recorded earthquakes. Finally, the frequency of oscillation of the Earth's magnetic field that could be associated with earthquakes is calculated and being consistent to the ultra-low frequency (ULF) signals that some authors propose in the so-called "LAIC Effect" (lithosphere-atmosphere-ionosphere coupling).
Abstract. This publication highlights theoretical work that could explain five
different empirical observations indicating a direct relationship between
magnetic fields and earthquakes, which would allow the description of a
causal mechanism prior to and during the occurrence of earthquakes. These
theoretical calculations seek to elucidate the role of the magnetic field in
different aspects of solid Earth dynamics, with an interest in the study and
comprehension of the physics that could generate earthquakes accompanied by
simultaneous magnetic signals within the lithosphere. The motion of charged
edge dislocations (MCD) model and its correlation with the magnetic field
have been used in order to include the generation of electric currents. The
electric currents resulting from stress variation in the lithosphere help
us to analyze the lithosphere as a critical system, before and after the
occurrence of earthquakes, by using the concept of earthquake entropy. Where
it is found that the nonexistence of seismic and magnetic precursors could
be interpreted as a violation of the second law of thermodynamics. In
addition, the seismic moment and the moment magnitude of some great
earthquakes are quite accurately calculated using the coseismic magnetic
field. The distance-dependent coseismic magnetic field has been theorized
for some of the largest recorded earthquakes. The frequency of oscillation
of the Earth's magnetic field that could be associated with earthquakes is
calculated and is consistent with the ultra-low-frequency (ULF) signals
that some authors propose in the so-called “LAIC effect”
(lithosphere–atmosphere–ionosphere coupling). Finally, the location and
dimensions of the microcracks that explain some anomalous magnetic
measurements are shown.
scite is a Brooklyn-based organization that helps researchers better discover and understand research articles through Smart Citations–citations that display the context of the citation and describe whether the article provides supporting or contrasting evidence. scite is used by students and researchers from around the world and is funded in part by the National Science Foundation and the National Institute on Drug Abuse of the National Institutes of Health.