Gumiel Garrido, P.Campos Egea, R.Hernández, J. R.Paredes, C.2016-11-212016-11-211996http://hdl.handle.net/10272/12860This 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 depositsspaAtribución-NoComercial-SinDerivadas 3.0 Españahttp://creativecommons.org/licenses/by-nc-nd/3.0/es/FractalGeometryVeinsMineralizationTungstenTinUraniumApatiteFracturesConnectivityCaracterísticas 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 PCharacteristics of the fractal geometry of several mineralized vein systems at the Hercynian Massif. Their application to prospectivity. Part II: W, Sn, U and P mineralizationsjournal articleopen access