ON THE MILD AND WILD MECHANICAL ROUGHNESS OF THE LITHOSPHERE

The 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 seis...

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Autor principal:	Gudehus,Gerd
Lenguaje:	English
Publicado:	Universidad Católica de la Santísima Concepción 2012
Materias:	fractality lithosphere roughness
Acceso en línea:	http://www.scielo.cl/scielo.php?script=sci_arttext&pid=S0718-28132012000100005
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spelling	oai:scielo:S0718-281320120001000052012-08-27ON THE MILD AND WILD MECHANICAL ROUGHNESS OF THE LITHOSPHEREGudehus,Gerd fractality lithosphere roughness The 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.info:eu-repo/semantics/openAccessUniversidad Católica de la Santísima ConcepciónObras y proyectos n.11 20122012-01-01text/htmlhttp://www.scielo.cl/scielo.php?script=sci_arttext&pid=S0718-28132012000100005en10.4067/S0718-28132012000100005
institution	Scielo Chile
collection	Scielo Chile
language	English
topic	fractality lithosphere roughness
spellingShingle	fractality lithosphere roughness Gudehus,Gerd ON THE MILD AND WILD MECHANICAL ROUGHNESS OF THE LITHOSPHERE
description	The 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.
author	Gudehus,Gerd
author_facet	Gudehus,Gerd
author_sort	Gudehus,Gerd
title	ON THE MILD AND WILD MECHANICAL ROUGHNESS OF THE LITHOSPHERE
title_short	ON THE MILD AND WILD MECHANICAL ROUGHNESS OF THE LITHOSPHERE
title_full	ON THE MILD AND WILD MECHANICAL ROUGHNESS OF THE LITHOSPHERE
title_fullStr	ON THE MILD AND WILD MECHANICAL ROUGHNESS OF THE LITHOSPHERE
title_full_unstemmed	ON THE MILD AND WILD MECHANICAL ROUGHNESS OF THE LITHOSPHERE
title_sort	on the mild and wild mechanical roughness of the lithosphere
publisher	Universidad Católica de la Santísima Concepción
publishDate	2012
url	http://www.scielo.cl/scielo.php?script=sci_arttext&pid=S0718-28132012000100005
work_keys_str_mv	AT gudehusgerd onthemildandwildmechanicalroughnessofthelithosphere
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ON THE MILD AND WILD MECHANICAL ROUGHNESS OF THE LITHOSPHERE

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