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Forms of Uniaxial
Interference Figures
Prathamesh S. Pawar
M.Sc. (I) Geology,
Dept of Geology,
S. P. Pune University
Nomenclature
• Isogyres: black bars which form the cross
• Melatope: intersection of the two isogyres.
It is the point from
where the optic
axis emerges.
• Colour bands are
called as
isochromes.
Interference
colours increase in
order outward from
the melatope, near
melatope colours
are low first order.
Forms or Types of Uniaxial Interference
Figures
• 3 types – Based on the orientation of optic
axis, which is analogous the orientation of the
mineral section
1. Optic Axis or Centred Figure
2. Off-Centred Figure
3. Optic Normal or Flash Figure
1. Optic Axis Figure
• aka Centered Interference Figure
• The isogyres form a perfect cross
• Melatope is perfectly centered
• Optic axis is vertical
• Interference figure for the mineral does not
move as the stage is rotated
Some examples of centered uniaxial
interference figures
Calcite Quartz
2. Off-cantered Figure
• Cross is not centered
• Melatope may or may not lie outside the field
of view
• Optic axis is not vertical
• On rotation the melatope swings in a circle
around the centre
If the Melatope is well out outside the field of
view the isogyres sweep across the field of
view in sequence as the stage is rotated - with
the isogyres always remaining parallel to the
crosshairs.
Some examples of of-centered uniaxial
interference figures
3. Optic Normal Figure
• aka Flash figure
• optic axis
horizontal
• The interference
figure produced is
very broad, fuzzy
and occupies most
the field of view
Thank You…

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Forms of Uniaxial Interference Figures Explained

  • 1. Forms of Uniaxial Interference Figures Prathamesh S. Pawar M.Sc. (I) Geology, Dept of Geology, S. P. Pune University
  • 2. Nomenclature • Isogyres: black bars which form the cross • Melatope: intersection of the two isogyres. It is the point from where the optic axis emerges. • Colour bands are called as isochromes. Interference colours increase in order outward from the melatope, near melatope colours are low first order.
  • 3. Forms or Types of Uniaxial Interference Figures • 3 types – Based on the orientation of optic axis, which is analogous the orientation of the mineral section 1. Optic Axis or Centred Figure 2. Off-Centred Figure 3. Optic Normal or Flash Figure
  • 4. 1. Optic Axis Figure • aka Centered Interference Figure • The isogyres form a perfect cross • Melatope is perfectly centered • Optic axis is vertical • Interference figure for the mineral does not move as the stage is rotated
  • 5.
  • 6. Some examples of centered uniaxial interference figures Calcite Quartz
  • 7. 2. Off-cantered Figure • Cross is not centered • Melatope may or may not lie outside the field of view • Optic axis is not vertical • On rotation the melatope swings in a circle around the centre
  • 8. If the Melatope is well out outside the field of view the isogyres sweep across the field of view in sequence as the stage is rotated - with the isogyres always remaining parallel to the crosshairs.
  • 9. Some examples of of-centered uniaxial interference figures
  • 10. 3. Optic Normal Figure • aka Flash figure • optic axis horizontal • The interference figure produced is very broad, fuzzy and occupies most the field of view