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

  1. P. Gumiel 1
  2. R. Campos 2
  3. J.R. Hernández 1
  4. C. Paredes 3
  1. 1 ITGE, Ríos Rosas 23, 28003, Madrid
  2. 2 CIEMAT, Avda Complutense, 22, 28040, Madrid
  3. 3 ETSIM, Rios Rosas 21, 28003, Madrid
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Revista:
Geogaceta

ISSN: 0213-683X

Año de publicación: 1996

Número: 20

Páginas: 1401-1404

Tipo: Artículo

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Otras publicaciones en: Geogaceta

Resumen

This 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 (D) and mass dimension (D) were obtained using Box-counting and Mass aggregation techniques. The /ater (D) 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 deposits.

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