Características de la geometría fractal de varios sistemas filonianos mineralizados del Macizo Hespérico. Su aplicación a la prospección: Parte II: Mineralizaciones de W, Sn, U y P

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dc.contributor.authorGumiel Garrido, P.
dc.contributor.authorCampos Egea, R.
dc.contributor.authorHernández, J. R.
dc.contributor.authorParedes, C.
dc.date.accessioned2016-11-21T11:39:18Z
dc.date.available2016-11-21T11:39:18Z
dc.date.issued1996
dc.description.abstractThis work is an atempt to characterize different vein sets with W, Sn, U, P (Part II) mineralizations of the Hercynian Massif, studying their internal organization and distribution. One-dimensional analysis of each vein sets has been carried out in Traverses. As a result of a two-dimensional analysys carried out from digitalization of several veins sets, other fractal dimensions as capacity dimension (DJ and mass dimension (Dm) were obtained using Box-counting and Mass aggregation techniques. The later (Dc) and (D ) values support the analysis of vein sets along Traverses in outcrops. The application of this methodology may play an important role in prospectivity of vein-type depositsen_US
dc.identifier.urihttp://hdl.handle.net/10272/12860
dc.language.isospaen_US
dc.publisherSociedad Geológica de Españaen_US
dc.rightsAtribución-NoComercial-SinDerivadas 3.0 España*
dc.rights.accessRightsopen accessen_US
dc.rights.urihttp://creativecommons.org/licenses/by-nc-nd/3.0/es/*
dc.subject.otherFractalen_US
dc.subject.otherGeometryen_US
dc.subject.otherVeinsen_US
dc.subject.otherMineralizationen_US
dc.subject.otherTungstenen_US
dc.subject.otherTinen_US
dc.subject.otherUraniumen_US
dc.subject.otherApatiteen_US
dc.subject.otherFracturesen_US
dc.subject.otherConnectivityen_US
dc.titleCaracterísticas de la geometría fractal de varios sistemas filonianos mineralizados del Macizo Hespérico. Su aplicación a la prospección: Parte II: Mineralizaciones de W, Sn, U y Pen_US
dc.titleCharacteristics of the fractal geometry of several mineralized vein systems at the Hercynian Massif. Their application to prospectivity. Part II: W, Sn, U and P mineralizationseng
dc.typejournal articleen_US
dspace.entity.typePublication

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Geogaceta -- Nº 20-6, (1996)