- This page is about the geology/optical mineralogy term. For general information about interference, see Interference (wave propagation) or Interference patterns.
A
conoscopic interference pattern or
interference figure is a pattern of
birefringent colours crossed by dark bands (or
isogyres), which can be produced using a
geological petrographic microscope for the purposes of
mineral identification and investigation of
mineral optical and chemical properties. The figures are produced by
optical interference when diverging light rays travel through an optically non-isotropic substance - that is, one in which the substance's
refractive index varies in different directions within it. The figure can be thought of as a "map" of how the birefringence of a mineral would vary with viewing angle away from perpendicular to the slide, where the central colour is the birefringence seen looking straight down, and the colours further from the centre equivalent to viewing the mineral at ever increasing angles from perpendicular. The dark bands correspond to positions where
optical extinction (apparent isotropy) would be seen. In other words, the interference figure presents all possible birefringence colours for the mineral at once.
