Optical Mineralogy Flashcards
Isometric crystal system
Axes: 3 Angles: 3 at 90 degrees Sides: a1 = a2 = a3 Optical properties: isotopic Optic axes: infinite
Hexagonal crystal system
*EXTINCTION: Parallel Axes: 4 Angles: 3 at 60 degrees Sides: a1 = a2 = a3 != c Optical properties: UNIaxial (type of anisotropy) Optic axes: 1
Tetragonal crystal system
*EXTINCTION: Parallel Axes: 3 Angles: 3 at 90 degrees Sides: a1 = a2 != c Optical properties: UNIaxial (type of anisotropy) Optic axes: 1
Orthorhombic crystal system
**EXTINCTION: Parallel Axes: 3 Angles: 3 at 90 degrees Sides: a != b != c **Optical properties: BIaxial (type of anisotropy) **Optic axes: 2
Monoclinic crystal system
*EXTINCTION: Angular Axes: 3 Angles: 2 at 90 degrees Sides: a != b != c Optical properties: BIaxial (type of anisotropy) Optic axes: 2
Triclinic crystal system
*EXTINCTION: Angular Axes: 3 Angles: 0 at 90 degrees Sides: a != b != c Optical properties: BIaxial (type of anisotropy) Optic axes: 2
Uniaxial optical properties & associated crystal systems
Uniaxial = 1 optic axis
(Type of anisotropy)
Angle size varies # of angles = 3 Axis c length != axes a’s # of axes varies
Uniaxial —> parallel extinction
BUT, not the other way around!
Parallel extinction != uniaxial (b/c orthorhombic is biaxial, but has parallel extinction)
Biaxial optical properties & associated crystal systems
Biaxial = 2 optic axes
(Type of anisotropy)
# of axes: 3 Lengths of axes: ALL UNEQUAL Angle size: varies (n/a or 90 degrees) # of angles = varies (0-3)
Angular extinction —> biaxial
BUT, not the other way around!
Biaxial != angular extinction (b/c orthorhombic is biaxial, but has parallel extinction)
Constructive interference
Light waves w/similar behaviors interact & combine resulting in AMPLIFIED light wave
Destructive interference
Light waves that are opposite/off interact & cancel each other out —> no light waves
Opaque minerals
No light passes through the mineral, regardless of sample thickness
Isotopic
Isotopic = infinite optic axes
Speed of light is equal in all directions
Anisotropic
Cause of extinction
In most directions, light splits into two rays w/two different speeds; vibrating at RIGHT angles
Uniaxial/biaxial: only specific directions: light isn’t split, i.e. behaves isotropically in specific directions
When optic axes are aligned with cross hairs of microscope: extinction occurs!
Amphibole vs. pyroxene, in thin section
Amphibole:
- 60/120 degrees
- double chain
- WIDER I-beam structure b/c of A site and OH
Pyroxene:
- 90/90 degrees
- single chain
Pleochroism
Change in colors as mineral is rotated on stage in PPL