Fractal clustering as spatial variability of magnetic anomalies measurements for impending earthquakes and the thermodynamic fractal dimension

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dc.catalogadorpva
dc.contributor.authorVenegas Aravena, Patricio
dc.contributor.authorCordaro, Enrique Guillermo
dc.contributor.authorLaroze, David
dc.date.accessioned2023-09-04T13:43:03Z
dc.date.available2023-09-04T13:43:03Z
dc.date.issued2022
dc.date.updated2023-09-02T22:16:06Z
dc.description.abstractSeveral studies focusing on the anomalies of one specific parameter (such as magnetic, ionospheric, radon release, temperature, geodetic, etc.) before impending earthquakes are constantly challenged because their results can be regarded as noise, false positives or are not related to earthquakes at all. This rise concerns the viability of studying isolated physical phenomena before earthquakes. Nevertheless, it has recently been shown that all of the complexity of these pre-earthquake anomalies rises because they could share the same origin. Particularly, the evolution and concentration of uniaxial stresses within rock samples have shown the generation of fractal crack clustering before the macroscopic failure. As there are studies which considered that the magnetic anomalies are created by lithospheric cracks in the seismo-electromagnetic theory, it is expected that the crack clustering is a spatial feature of magnetic and non-magnetic anomalies measurements in ground, atmospheric and ionospheric environments. This could imply that the rise of multiparametric anomalies at specific locations and times, increases the reliability of impending earthquake detections. That is why this work develops a general theory of fractal-localization of different anomalies within the lithosphere in the framework of the seismo-electromagnetic theory. In addition, a general description of the fractal dimension in terms of scaling entropy change is obtained. This model could be regarded as the basis of future early warning systems for catastrophic earthquakes.
dc.fechaingreso.objetodigital2023-09-02
dc.fuente.origenAutoarchivo
dc.identifier.doi10.3390/fractalfract6110624
dc.identifier.urihttps://doi.org/10.3390/fractalfract6110624
dc.identifier.urihttps://repositorio.uc.cl/handle/11534/74570
dc.identifier.wosidWOS:000881084300001
dc.information.autorucEscuela de ingeniería ; Venegas Aravena, Patricio ; S/I ; 1080976
dc.issue.numero11
dc.language.isoen
dc.nota.accesoContenido completo
dc.pagina.final13
dc.pagina.inicio1
dc.revistaFractal Fractes_ES
dc.rightsacceso abierto
dc.rights.licenseAttribution 4.0 International (CC BY 4.0)
dc.rights.urihttps://creativecommons.org/licenses/by/4.0/
dc.subjectSeismic clusteringes_ES
dc.subjectFractal cracking localizationes_ES
dc.subjectSeismo-electromagnetic theoryes_ES
dc.subjectLithosphere–atmosphere–ionosphere couplinges_ES
dc.subjectThermodynamic fractal dimensiones_ES
dc.subject.ddc620
dc.subject.deweyIngenieríaes_ES
dc.subject.ods13 Climate action
dc.subject.odspa13 Acción por el clima
dc.titleFractal clustering as spatial variability of magnetic anomalies measurements for impending earthquakes and the thermodynamic fractal dimensiones_ES
dc.typeartículo
dc.volumen6
sipa.codpersvinculados1080976
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