Article ID | Journal | Published Year | Pages | File Type |
---|---|---|---|---|
8914468 | Journal of Structural Geology | 2018 | 56 Pages |
Abstract
Variation of spatial correlation with length scale, and interpretation of some patterns (a-h). x-axis is linear in a through d, logarithmic in e through h. (a) A flat-line pattern of spatial correlation (slope = 0; correlation = 1) indicates no statistically significant organization. (c, d, h) Periodic peaks and troughs (best appreciated with linear graduations of length scale) indicate regular spacing, another form of self organization. Combinations of any or all of these patterns can occur, with different patterns characterizing different ranges of length scale. (b) Individually anti-clustered but not regularly spaced. (f-h) Power-law variation of spatial correlation with length scale (slope â 0; best appreciated with logarithmic graduations of length scale) indicates fractal clustering, one form of self organization. (e) A plateau-and-basin pattern of spatial correlation (slope = 0; correlation â 1) indicates statistically significant clustering, due to some process other than self organization such as inherited or externally imposed control. Column colors mark linear and log scales.213
Related Topics
Physical Sciences and Engineering
Earth and Planetary Sciences
Geology
Authors
Randall Marrett, Julia F.W. Gale, Leonel A. Gómez, Stephen E. Laubach,