Fig. 9. Oriented remnant fragments of plagioclase (white, light gray) in zoned megacryst of microcline (dark gray). Remnant fragments of plagioclase that are not parallel to a possible crystal face of the microcline tend to have scalloped edges and veins of microcline extending into the plagioclase. Myrmekite forms border (left side) of disoriented plagioclase inclusions on right side of photo.