Figure 8From: Characterization of olivine fabrics and mylonite in the presence of fluid and implications for seismic anisotropy and shear localizationBackscattered electron images showing dislocation microstructures of olivine. Dislocations are shown as white dots and lines. (A) Homogeneous distribution of dislocations in olivine in the large-grained area (sample 372). E-type LPOs are observed from sample 372. (B) Magnified view of Figure 8A. Straight dislocations are observed. (C) Homogeneous distribution of dislocations in olivine in the large-grained area (sample 373). A combination of A- and B-type LPOs are observed. (D) Magnified view of Figure 8C. (E) Dislocation of olivine in the medium-grained area in mylonite (sample 380). (F) Magnified view of Figure 8E. (G) Heterogeneous distribution of dislocations in olivine in the small-grained area in mylonite (sample 380). (H) Four-grain junctions (yellow arrows) found in the small-grained area in mylonite (sample 379).Back to article page