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Scaling in granitic geological media

dc.contributor.authorParedes, C.
dc.contributor.authorChacón, E.
dc.contributor.authorElorza, Javier
dc.date.accessioned2016-11-17T11:33:44Z
dc.date.available2016-11-17T11:33:44Z
dc.date.issued1996
dc.identifier.urihttp://hdl.handle.net/10272/12845
dc.description.abstractIts easy to aprecíate that the fracture field creates a tortuous pipe networks. Such nets usually have an scaling or fractal structure, in most of the cases studied, and some spatial distribution properties which allow us to characterize them as fractals. This hard task is made to simulate the hidrogeological behaviour in the fractured media. Really, the problem arises when one wants to do a fractal characterization and simulation both related. Thats is the problem dealed in this work. Two difieren ways of analyses (an Inverse Box-Counting Method MIBC, and an aggregation mass algorithm) related with two fractal simulation methodologies, to describe and simulate the fractaiity in fracture nets, are exposed, and showed With an example which uses the El Berrocal data baseen_US
dc.language.isospaen_US
dc.publisherSociedad Geológica de Españaen_US
dc.rightsAtribución-NoComercial-SinDerivadas 3.0 España*
dc.rights.urihttp://creativecommons.org/licenses/by-nc-nd/3.0/es/*
dc.subject.otherFractal analysisen_US
dc.subject.otherFractal simulationen_US
dc.subject.otherFracture distributionen_US
dc.subject.otherGranitic mediaen_US
dc.titleAnálisis y simulación fractal de medios graníticosen_US
dc.titleScaling in granitic geological mediaeng
dc.typeinfo:eu-repo/semantics/articleen_US
dc.rights.accessRightsinfo:eu-repo/semantics/openAccessen_US


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