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

• P. Gumiel ^[1] ; R. Campos ^[2] ; J.R. Hernández ^[1] ; 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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• Localización: Geogaceta, ISSN 0213-683X, Nº. 20, 6 (Comunicaciones presentadas en el IV Congreso Nacional de Geología, Alcalá de Henares, 1996), 1996, págs. 1401-1404
• Idioma: español
• Títulos paralelos:
  • Characteristics of the fractal geometry of several mineralized vein systems at the Hercynian Massif. Their application to prospectivity. Part II: W, Sn, U and P mineralizations
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• 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.