RT Journal Article
T1 Sistemas filonianos multifractales en la Península Hurd, Isla Livingston, Antártida Occidental
A1 Gumiel, P.
A1 González-Casado, J.M.
A1 Giner Robles, Jorge Luis
A1 López-Martínez, J.
A1 Durán, J.J.
AB Analysis of vein systems has been carried out in eleven traverses along the coastal area on Hurd Peninsula, Livingston Island (South Shetland Islands, Western Antarctica), to characterise vein geometry using fractal and multifractal analysis techniques. Vein thicknesses generally conform to a power law distribution of the form N(k C t D, where Nt is the number of veins with a  thickness > t. This may be interpreted in terms of scale-invariant (self-affine fractal scaling of vein geometry) which has been verified to several orders of magnitude. Multifractal analysis of vein networks has been applied using the capacity dimension (D J, the information dimension  (Dt) and the correlation dimension (D ,) to measure the heterogeneity, dimensionality and connectivity of the fracture systems.
PB Sociedad Geológica de España
SN 1576-5172
YR 2000
FD 2000
LK https://hdl.handle.net/20.500.14352/107325
UL https://hdl.handle.net/20.500.14352/107325
LA spa
NO Gumiel Martínez, P. et al. (2000): «Sistemas filonianos multifractales en la Península Hurd, Isla Livingston, Antártida Occidental», Geotemas (Madrid), 1, pp. 181-184.
NO Comisión Interministerial de Ciencia y Tecnología (España)
DS Docta Complutense
RD 17 abr 2025