OPTICAL MINERALOGY AND PETROGRAPHY (CONOSCOPIC UNIAXIAL) Flashcards

1
Q

Conoscopic Setup

A

Light Source In
Polarize In
Condenser In
HIGHEST POWERED OBJECTVE
Analyzer In
Bertrand Lens IN

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2
Q

Without Bertrand Lends, How can IF be observed?

A

Remove Ocular or
Insert Pinhole Ocular

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3
Q

A combination of EXTINCTION and INTERFERENCE COLORS Produced by rays going through the sample at different angles which consists of STRONGLY CONVERGING LIGHTS under the conoscopic illumination

A

Interference Figure

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4
Q

Uses of Interference figure

A

Distinguish between Uniaxial and Biaxial
Determine Optic Sign

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5
Q

Two arms of the cross in N-S, E-W direction where vibration are perpendicular

A

Isogyres

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6
Q

The point where isogyres corss and where the optic axis emerges in the interference figure

A

Melatope

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7
Q

Bands of Equal retardation which increases from the center or
Interferece colors indentical to those on the colour char increases order from the melatope outwards

A

Isochromes

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8
Q

?Circular/Basal Section
?Vertical Optic Axis
?centred black cross superimposed on circular bands of Int. Colors
?Does not move when stage is rotated (Stationary)
?Since optical Axis is vertical, optical properties vary symmetrically
?Number of isochromes depends on retardation and thickness
?Birefringence 0

A

Centered Optic Axis Figure

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9
Q

In a centered optic axis the Ordinary ray (w) vibrates in what direction
Like Latitude on the surface of the indicatrix

A

PERPENDICULAR to the C-axis conincides with the isochrome

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10
Q

In a centered optic axis the Extraordinary (e) ray vibrates in what direction
Like Longitude on the surface of the indicatrix

A

PARALLEL or RADIAL to the C-axis

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11
Q

?Random Section
?Melatope lies outside the FOV the isogyre fattens as the distance from the melatope increases
?Optic axis is not vertical
?On rotation, melatope swing in a circle around the center of the field of view
?Birefringence is intermediate

A

Off Centered Optic Axis Figure

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12
Q

?Mineral grain is oriented with its optic axis horizontal
?Birefringence is Maxmimum
?result because vibration of the directions are nearly parallel to the polarisation of the microscope
?Horizontal or Principal Section

A

Uniaxial Flash Figure

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13
Q

When will the isogyre cross be split in two and rapidly leave the FOV in the quadrants into which the Optic Axis is aligned

A

<5 deg rotation rotation

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14
Q

at this position no isogyres will be present and the field of view may exhibit some interference colors or isochromes

A

<10 deg rotation

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15
Q

Optically Positive

A

w=fast e=slow

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16
Q

Optically negative

A

w=slow e=fast

17
Q

Set up to determine optic sign

A

Conoscopic with Centered Optic Axis
Insert Gypsum Plate (Compensator)
Look at the NE quadrant of the interference figure

18
Q

Why NE Quadrant

A

It corresponds to the Extraordinary Ray Vibration

19
Q

If the interference color of the isochrome in the NE quadrant increases in order (Yellow to blue), the Extraordinary wave is the slow ray

A

Optically positive

20
Q

If the interference color in the NE quadrant decreases Blue to yellow, the extraordinary ray is the fast ray

A

Optically Negative

21
Q

Using quartz wedge if the ischromes move outward away from the melatope (NE-SW)

A

Optically Negative

22
Q

Using quartz wedge if the isochromes move inwards towards the melatope (NE-SW Direction)

A

Optically Positive