Abstract
Digitised outlines of a serially sectioned K-feldspar grain from a Cordilleran granitoid have been analysed for their fractal dimension. Each grain section has fractal dimension (D) >1, ranging from 1.21-1.30. Scatter within the data sets have been used to define separate (pseudo)fractal elements that further characterise each grain outline. The development of fractal geometries within a particular granitoid can be broadly related to crystallisation within Ab-An-Or-Qz space. The non-integer values that describe grain shape may be useful in estimating the total grain (porosity) volume within the rock. -from Authors
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CITATION STYLE
Petford, N., Bryon, D., Atherton, M. P., & Hunter, R. H. (1993). Fractal analysis in granitoid petrology: a means of quantifying irregular grain morphologies. European Journal of Mineralogy, 5(3), 593–598. https://doi.org/10.1127/ejm/5/3/0593
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