REPRESENTING PROGRESSIVE FABRIC PATHS ON A TRIANGULAR PLOT USING A FABRIC DENSITY INDEX AND CRYSTAL AXES EIGENVECTOR BARYCENTERS
An alternative measure of fabric strength, based on the Bingham test statistic for uniformity, is the fabric intensity index:
I = (15/2) Σ[ε - 1/3]2
which ranges from 0 to 5 (Lisle 1985, Vollmer 1990). The end members are: uniform I = 0, girdle I = 1.25, and cluster I = 5. I is a measure of the "squared distance" from uniformity, and is non-linear. Therefore a fabric density index is proposed:
D = √[(3/2) Σ[ε - 1/3]2]
D is a measure of the "distance" from uniformity, and is linear from R to P, and R to G. End members are: uniform D = 0, girdle D = 0.5, cluster D = 1. The 99% level for a test against uniformity for a sample size of 300 is D = 0.1.
A single axis, as the c-axis of quartz, may be used to characterize a fabric. An example is from mylonitic quartz CPOs collected along a 9.5 km transect across the Main Central Thrust, Himalaya (Hunter et al. 2019). The progressive fabric path forms a loop across the shear zone with D increasing into the shear zone.
The full crystal orientation may be described by three axes, such as for olivine. End members are: uniform, one cluster with two girdles, and three clusters. Three girdles are not possible. Fabric indexes can be defined using the axes eigenvector barycenter:
εB = (1/3)(ε[100] + ε[010] + ε[001])
End members are: uniform [PB, GB, RB] = [0, 0, 1], one cluster with two girdles [1/3, 2/3, 0], and three clusters [1, 0, 0]. An example is from experimentally deformed olivine (Hansen et al. 2014). The progressive fabric path forms a curve from near R towards P, along which D increases with shear strain.
An implementation with example data is provided in the free software Orient, available from the author's website: https://vollmerf.github.io