Sobre la suave y salvaje rugosidad mecánica de la litósfera
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https://doi.org/10.4067/S0718-28132012000100005Palabras clave:
Fractalidad, Litósfera, RugosidadResumen
La fractalidad mecánica espacio-temporal de la litósfera puede ser representada por medio de la estadística de Lévy y cálculo fraccional. Este nuevo concepto es planteado con argumentos geométricos y energéticos. La fractalidad se origina del sistema poroso y aparece en desplazamientos, tensiones y sismicidad. Se muestra que la rugosidad podría no ser considerada en el rango estable, pero esto no es posible en fenómenos críticos al borde de convexidad energética. Este planteamiento cubre bordes costeros rugosos, muestras de arena y reacciones tectónicas en cadena. Ecuaciones y teoremas son interpretados físicamente sin la necesidad de álgebra ni pruebas.
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Derechos de autor 2012 Universidad Católica de la Santísima Concepción
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