Abstract
The capacity of fractal statistics to describe the geometry of mineralized vein systems has been tested for a series of molybdenite- and chalcopyrite-bearing quartz veins at Mace Head, County Galway. Vein thicknesses are described best by a power-law distribution and vein spacings by a log-normal distribution. Vein lengths and thicknesses are also related to each other by a power-law distribution. This relationship may be a product of non-linear amplification of initially randomly spaced veins and causes outcrop-scale veins to be relatively more elongate than on a map. This self-affine fractal geometry is reflected in vein size distributions and can be used as a predictive tool. -from Authors
| Original language | English |
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| Pages (from-to) | 139-148 |
| Number of pages | 10 |
| Journal | Irish Journal of Earth Sciences |
| Volume | 12 |
| Publication status | Published - 1993 |