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Lecture 16 (11/20/2006) Analytical Mineralogy Part 3: Optical Properties of Biaxial Minerals
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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
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Biaxial Indicatrix Principal vibration axes n greatest n n lowest n n intermediate n < ’<<’<
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Circular Sections and Optic Axes Circular Section OpticAxes OpticPlane
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2V and the Optic Sign + - Trace of Circular Sections
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Random Section through the Biaxial Indicatrix Vibration plane parallel to stage Double refraction rays
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Variable Birefringence within a Biaxial Mineral =0 =max
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Biaxial Optic Axis Figures Look for a mineral with the lowest interference colors, i.e. ~0
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Acute Bisectrix Figures (Bxa) Melatope (emergence of optic axes)
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Off-centered Bxa figure
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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
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Estimating 2V by Curvature of Isogyre
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Estimating 2V by Separation of Isogyres
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Extinction Angle Symmetrical ParallelInclined
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Sign of Elongation slowray Example – Length slow Interference colors increase Slowing down the slow ray
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Next Lecture 11/22/06 Principles of X-ray Mineralogy Read: Klein p. 309-321
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