Figure 1From: Subgrain boundary analyses in deformed orthopyroxene by TEM/STEM with EBSD-FIB sample preparation techniqueCross-polarized optical micrograph of the petrographic thin section of mylonite rock cut in the X - Z plane. The pole to foliation is indicated by Z-axis, and the lineation is indicated by X-axis. Spindle-like large grains are Opx porphyroclast, and the matrix is mostly made of plagioclase.Back to article page