Identification of Minerals Flashcards

1
Q

Observations during PPL

A

Opacity
Habit, Form, mode of aggregation
Color
Pleochroism
Cleavage

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2
Q

Observations during XPL

A

Isotropic vs Anisotropic
Habit
Cleavage
Interference color
Sign of elongation
Extinction and ext angles
Twinning, zoning

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3
Q

Function of the wavelength transmitted by the mineral

A

Color

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4
Q

Color is best observed in?

A

PPL

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5
Q

the ability of a mineral to absorb different wavelengths of transmitted light depending upon its crystallographic orientation.

A

Pleochroism

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6
Q

Pleochroic hexagonal and tetragonal minerals

A

twofold pleochroism; dichroic

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7
Q

exhibit varying degrees of absorption

A

Biaxial minerals

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8
Q

Exhibit three different colors

A

trichroic

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9
Q

darkest at long axis oriented perpendicular to polarizer

A

“normal” pleochroism

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10
Q

darkest at long axis oriented parallel to polarizer

A

“reverse” pleochroism

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11
Q

The degree to which mineral grains stand out from the mounting medium, have sharp boundaries, show fractures and cleavages well

A

Relief

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12
Q

without regular crystal faces

A

anhedral

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13
Q

has well-formed crystal faces

A

euhedral

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14
Q

elongate needlelike grains

A

acicular

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15
Q

elongate, slender

A

bladed

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16
Q

shaped like a column

A

columnar

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17
Q

equidimensional grains

A

equant

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18
Q

individual grains are long slender fibers

A

fibrous

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19
Q

flat elongate grains

A

lathlike

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20
Q

the dominant faces are those of a prism

A

prismatic

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21
Q

shaped like a book

22
Q

more or less parallel tabular or platy grains; flaky

23
Q

equant grains, all about the same size

24
Q

elongate grains in a random pattern

25
elongate grains that radiate out from a center
radiating
26
the way a mineral splits in preferred directions
Cleavage
27
Things to do when looking for cleavage
Determine angle characterize if perfect, good, or weak/poor
28
- Light rays are parallel to wave normal - Shows same velocity of light in all directions - Bonds are the same in all directons
Isotropic minerals
29
- Light rays are not parallel to wave normal - Shows different velocity of light in all directions - Bonds are not the same in all directions
Anisotropic minerals
30
The wavelength (color) exhibited by a mineral when viewed under XPL
Interference color
31
dependent on orientation of mineral, or presence of cleavages of mineral grain
Extinction
32
maximum interference angle that could be observed
45 degrees
33
Monoclinic and triclinic minerals show what type of extinction
inclined extinction
34
All uniaxial minerals show what type of extinction
Parallel extinction
35
36
no cleavage to base extinction from
No extinction angle
37
different parts of a grain becomes extinct at different angles
undulose/undulatory extinction
38
The distance that one wave lags behind the other
Retardation
39
Where i is an integer, then the two waves are said to be in phase
constructive interference
40
two waves are said to be out of phase
destructive interference
41
to determine which of the two rays coming through the mineral is the slow ray and which is the fast ray
sign of elongation
42
fast ray direction
NW-SE
43
slow ray direction
NE-SW
44
3 ways to determine the sign of elongation
Orient the elongated mineral at 45 degrees CW Note interference color Engage compensator
45
If increase in IC, mineral is length ____, or _____
length-slow; positive elongation
46
If decrease in IC, mineral is ____; or_____
length-fast; negative elongation
47
if mineral has 1 degree white gray IC, what plate should be used
mica plate
48
color blind users use what plate
quartz wedge
49
the intergrowth of two or more crystals in a symmetrical fashion by the sharing of lattice points in adjacent crystals
twinning
50
changes smoothly from a more calcic core to a more sodic rim
normal zoning