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Lecture 16 (11/20/2006) Analytical Mineralogy Part 3: Optical Properties of Biaxial Minerals.

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Presentation on theme: "Lecture 16 (11/20/2006) Analytical Mineralogy Part 3: Optical Properties of Biaxial Minerals."— Presentation transcript:

1 Lecture 16 (11/20/2006) Analytical Mineralogy Part 3: Optical Properties of Biaxial Minerals

2 Optical Indicatrices A 3-d map of the indices of refraction for various vibration directions of light rays Orientation of the indicatrix within a mineral is symmetrical with the crystallographic axis IsotropicIsometric Anisotropic – Uniaxial TetragonalHexagonal Anisotropic-BiaxialOrthorhombicMonoclinicTriclinic

3 Biaxial Indicatrix Principal vibration axes n greatest n n lowest n n intermediate n < ’<<’<

4 Circular Sections and Optic Axes Circular Section OpticAxes OpticPlane

5 2V and the Optic Sign + - Trace of Circular Sections

6 Random Section through the Biaxial Indicatrix Vibration plane parallel to stage Double refraction rays

7 Variable Birefringence within a Biaxial Mineral =0 =max

8 Biaxial Optic Axis Figures Look for a mineral with the lowest interference colors, i.e. ~0

9 Acute Bisectrix Figures (Bxa) Melatope (emergence of optic axes)

10 Off-centered Bxa figure

11 Determining the Optic Sign of Biaxial Minerals D + D - U U D D D D ’ is fast ray  is intermediate ’ is slow ray - + X X U U U U

12 Estimating 2V by Curvature of Isogyre

13 Estimating 2V by Separation of Isogyres

14 Extinction Angle Symmetrical ParallelInclined

15 Sign of Elongation slowray Example – Length slow Interference colors increase Slowing down the slow ray

16 Next Lecture 11/22/06 Principles of X-ray Mineralogy Read: Klein p. 309-321


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