Category
page 1Optical mineralogy

birefringence
right|thumb|A calcite crystal laid upon a graph paper with blue lines showing the double refraction
right|thumb|In this example, optic axis along the surface is shown perpendicular to plane of incidence. Incoming light in the polarization (which means perpendicular to plane of incidence – and so in this example becomes "parallel polarisation" to optic axis, thus is called extraordinary ray) sees a greater refractive index than light in the polarization (which becomes ordinary ray because "perpendicular polarisation" to optic axis) and so polarization ray is undergoing greater refraction on ent

petrography
Petrography is a branch of petrology that focuses on detailed descriptions of rocks. Someone who studies petrography is called a petrographer. The mineral content and the textural relationships within the rock are described in detail. The classification of rocks is based on the information acquired during the petrographic analysis. Petrographic descriptions start with the field notes at the outcrop and include macroscopic description of hand-sized specimens. The most important petrographer's tool is the petrographic microscope. The detailed analysis of minerals by optical mineralogy in thin se
pleochroism
thumb|Pleochroism of cordierite shown by rotating a polarizing filter on the lens of the camera
thumb|Pleochroism of tourmaline shown by rotating a polarizing filter on the lens of the camera

Waveplate
[[Image:Waveplate.png|thumb|300px|
petrographic microscope
optical microscope
thin section
laboratory preparation rock, mineral, soil, pottery, bones, metal for petrographic microscope
optic axis of a crystal
birefringence-free direction of light transmission
optical mineralogy
The optical properties of rocks and minerals
Becke line test
Conoscopic interference pattern
A pattern of birefringence colors
undulose extinction
geological term
index ellipsoid
aspect of crystal optics
extinction
term used in optical mineralogy and petrology