Please use this identifier to cite or link to this item: http://cmuir.cmu.ac.th/jspui/handle/6653943832/72901
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dc.contributor.authorRami Ahmad El-Nabulsien_US
dc.contributor.authorWaranont Anukoolen_US
dc.date.accessioned2022-05-27T08:31:16Z-
dc.date.available2022-05-27T08:31:16Z-
dc.date.issued2022-01-01en_US
dc.identifier.issn16196937en_US
dc.identifier.issn00015970en_US
dc.identifier.other2-s2.0-85129799213en_US
dc.identifier.other10.1007/s00707-022-03213-7en_US
dc.identifier.urihttps://www.scopus.com/inward/record.uri?partnerID=HzOxMe3b&scp=85129799213&origin=inwarden_US
dc.identifier.urihttp://cmuir.cmu.ac.th/jspui/handle/6653943832/72901-
dc.description.abstractIn this study, we constructed the seismic wave equation in fractal dimensions based on the concept of product-like fractal measure introduced recently by Li and Ostoja-Starzewski in their formulation of anisotropic media. The solutions of the fractal seismic wave have proved the effect of fractal dimensions on the propagation of this type of wave in anisotropic media. The plane wave solutions were proved to be affected and deformed by fractal dimensions. It was observed that earthquakes in fractal dimension are characterized by a modified total energy which may be used to estimate the range of the fractal dimension. In particular, slow earthquakes with fractal dimension α= 1 / 2 are characterized by a particular total energy Eα which is Eα≈ 10 Ec, Ec being the conventional total energy. Several additional points were discussed and analyzed.en_US
dc.subjectEngineeringen_US
dc.titleFractal dimension modeling of seismology and earthquakes dynamicsen_US
dc.typeJournalen_US
article.title.sourcetitleActa Mechanicaen_US
article.stream.affiliationsChiang Mai Universityen_US
article.stream.affiliationsAthens Institute for Education and Researchen_US
Appears in Collections:CMUL: Journal Articles

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