(6) Identification of minerals Flashcards

(53 cards)

1
Q

. function of the wavelength transmitted by the mineral

. best observed in PPL

A
  • color
  • may be colorless, weakly colored or strongly colored
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2
Q

the ability of a mineral to absorb different
wavelengths of transmitted light depending upon its ______

A

crystallographic orientation

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3
Q

used to describe the color variation for
destructive interferencewith the polarization direction of the light, which depends on the
orientation of the material in the light path

A

Pleochroism

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4
Q

colored uniaxial and biaxial are usually___

A

pleochroic

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5
Q

twofold pleochroism or DICHROIC

A

Pleochroic hexagonal and tetragonal minerals:

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6
Q

light vibrating at OA = color 1;
light at perpendicular to OA = color 2

A

Uniaxial minerals:

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7
Q

exhibit varying degrees of
absorption

A

Biaxial minerals:

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8
Q

exhibit three different colors; trichroic

A

Pleochroic orthorhombic, monoclinic and triclinic
minerals

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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

A

Relief

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12
Q

without
regular crystal faces

A

anhedral:

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13
Q

has wellformed crystal faces

A

euhedral

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14
Q

has
crystal faces but
they are poorly
formed or irregular

A

subhedral

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15
Q

elongate needlelike grains

A

acicular

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16
Q

elongate, slender

A

bladed

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17
Q

shaped like a column; moderately
elongate grains with equidimensional cross
section

A

columnar

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18
Q

equidimensional grains

A

equant

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19
Q

: individual grains are long slender fibers

A

fibrous

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20
Q

flat elongate grains

A

lathlike

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21
Q

shaped like a book

A

tabular

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22
Q

parallel arrangement of columnar
grains

23
Q

more or less parallel tabular or platy grains; flaky

24
Q

equant grains, all about the same
size

25
elongate grains in a random pattern
matted
26
elongate grains that radiate out from a center
radiating
27
-the way a mineral splits in preferred directions -represent planes of weak bonding in the mineral's atomic structure
Cleavage
28
Light rays are **parallel** to wave normal Shows **same** velocity of light in all directions Bonds are the **same** in all directions
Isotropic materials
29
examples of isotropic materials
isometric minerals and mineraloids
30
Light rays are **not parallel** to wave normal Shows **different** velocity of light in all directions Bonds are the **not the same** in all directions
anisotropic materials
31
anisotropic materials example
minerals in tetragonal, hexagonal, orthorhombic, monoclinic, and triclinic systems
32
The wavelength (color) exhibited by a mineral when viewed under XPL
Interference color
33
Dependent on orientation of mineral, or presence of cleavages of mineral grain
Extinction
34
All uniaxial minerals show what kind of extinction
parallel extinction
35
Orthorhombic minerals show what kind of extinction
parallel extinction
36
the crystal axes and indicatrix axes coincide
true (fun fact)
37
Monoclinic and triclinic minerals have what kind of extinction
inclined extinctions
38
FUN FACT
indicatrix axes **do not** coincide with crystallographic axes
39
different parts of a grain become extinct at different angles
Undulose/undulatory extinction:
40
: the distance that one wave lags behind the other (measured in nm)
Retardation
41
Light rays travelling along the same path will in the same direction will____
interfere with each other
42
tumaas yung interference color
constructive interference!
43
two waves are said to be out of phase
destructive interference!
44
If material with known retardation ΔA is superimposed over the mineral so that the slow ray vibration directions are parallel, the resulting slow ray and is further retarded
Higher interference color is produced
45
If mineral’s fast ray is parallel to the slow ray of the material with known retardation ΔA, slow ray of mineral becomes fast ray in material with known retardation ΔA mineral’s fast ray is retarded
Lower interference color is produced
46
The fast ray direction of the accessory plate is typically____
parallel to its length
47
fast ray is
NW-SE
48
slow ray is
NE-SW
49
if mineral has 1° white-gray IC
use mica plate
50
color blind users
use quartz wedge
51
the intergrowth of two or more crystals in a symmetrical fashion by the sharing of lattice points in adjacent crystals
twinning
52
changes smoothly from a more calcic core to a more sodic rim -core has a larger extinction angle
Normal zoning:
53
alternation between calcic and sodic zones -usually from a more calcic core to a more sodic rim.
Oscillatory zoning: