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dc.creatorGudehus,Gerd
dc.date2012-01-01
dc.date.accessioned2019-04-25T12:45:15Z
dc.date.available2019-04-25T12:45:15Z
dc.identifierhttps://scielo.conicyt.cl/scielo.php?script=sci_arttext&pid=S0718-28132012000100005
dc.identifier.urihttp://revistaschilenas.uchile.cl/handle/2250/61639
dc.descriptionThe spatio-temporal mechanical fractality of the lithosphere can be represented by means of Lévy-statistics and fractional calculus. This novel concept is outlined with geometrical and energetic arguments. The fractality originates from the pore system and appears in displacements, stresses and seismicity. It is shown that the roughness may be neglected for the stable range, but not for critical phenomena at the verge of energetic convexity. The outline leads from rough coastlines via sand samples to tectonic chain reactions. Equations and theorems are physically interpreted without algebra and proofs.
dc.formattext/html
dc.languageen
dc.publisherUniversidad Católica de la Santísima Concepción
dc.relation10.4067/S0718-28132012000100005
dc.rightsinfo:eu-repo/semantics/openAccess
dc.sourceObras y proyectos n.11 2012
dc.subjectfractality
dc.subjectlithosphere
dc.subjectroughness
dc.titleON THE MILD AND WILD MECHANICAL ROUGHNESS OF THE LITHOSPHERE


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