Single fracture aperture patterns: Characterization by slit-island fractal analysis Page: 3 of 11
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STRIPA FRAC
N = 0 0
- MaC = 159 05
Mean = 47 50
S D. = 38.95(
CV = 0.82 10
Skew = 1.80
Kurt = 2.70 (
N = 403 x 40?TURE
(I 10 0(
(37 00)
21.28)
58)
(1.01)
0.95)
3 (152,943U
ma
2U 40 0D '1C .Z 11
Aperture
Figure 1. Surface plots and histograms for Stripa (a) and Dixie
values removed,DIXIE VALLEY FRACTURE
Min = 0.0
Max = 241,28 (152.90)
Mean = 53.82 (41,95)
SD = 51.24 (20.92)
CV = 0.95 (0.50)
Skew = 2.88 (1.84)
Kurt = 7.66 (5.05)
N = 369 x 369 (128,014)I
lim 1%.0
Aperture0 0
Valley (b) fractures. Values in parentheses are statistics with the extreme
7C C 12 2" *2 %
Row Distance, mmCa
E:6.5 6 3
6 i. '2 29 57 ." 26
Row Distance, mmFigure 2. Profiles taken along row 150 for the Stripa (a) and Dixie Valley (b) fractures.
3 0
C0=
U
E:Stripa Fracture
Dixie Valley Fracture
fa 1 ..* 2. ) ! .
:,r ' ~ "a59 0,
4
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Cox, B.L. & Wang, J.S.Y. Single fracture aperture patterns: Characterization by slit-island fractal analysis, article, January 1, 1993; California. (https://digital.library.unt.edu/ark:/67531/metadc620513/m1/3/: accessed March 19, 2024), University of North Texas Libraries, UNT Digital Library, https://digital.library.unt.edu; crediting UNT Libraries Government Documents Department.