Mineralogy 1 Flashcards

(71 cards)

1
Q

arrange the oxides by weight:
Al2O3
CaO
TiO2
H2O
SiO2
MgO
K2O
Na2O
Fe2O3
FeO
Remaining oxides

A

SiO2
Al2O3
CaO
FeO
Na2O
MgO
K2O
Fe2O3
H2O
TiO2
Remaining oxides

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2
Q

olivine, garnet, zircon, kyanite are example of what tetrahedron configuration

A

Isolated (nesosilicates)

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3
Q

epidote, zoisite are example of what tetrahedron configuration

A

Pairs (sorosilicates)

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4
Q

Tourmaline is an example of what tetrahedron configuration

A

Rings (cyclosilicates)

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5
Q

pyroxenes, wollastonite are example of what tetrahedron configuration

A

single chains (inosilicates)

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6
Q

amphiboles are example of what tetrahedron configuration

A

double chains (inosilicates)

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7
Q

Micas, clay minerals, serpentine, chlorite are example of what tetrahedron configuration

A

sheets (phyllosilicates)

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8
Q

felds, quartz, zeolite are example of what tetrahedron configuration

A

framework (tectosilicates)

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9
Q

intergrowth of sodic and potassic felds resulting from subsolidus exosolution (unmixing of two minerals
has blebs or irregular lamellae of sodic feldspar within potassic alkali feldspar

A

Perthite

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10
Q

intergrowth of branching rods of quartz set in a single crystal of plag
derived from the ancient greek work “myrmekia” (wart)

A

Myrmekite

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11
Q

appearance of runic writing
suggested to originate by simultaneous crystallisation

A

Graphic Texture

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12
Q

solid solution phase umixes into two separate phases in the solid state

A

Exosolution lamellae in pyroxene

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13
Q

the same direction in all directions
(garnet, spinel)

A

equant

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14
Q

equant with a nearly square cross sections
(halite, galena)

A

blocky

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15
Q

needlelike
(actinolite, sillimanite)

A

acicular

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16
Q

plates or thick sheet
(gypsum, graphite)

A

tablular or platy

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17
Q

hairlike or threadlike (serpentine, millerite)

A

capillary or filiform

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18
Q

elongated and flatened in one direction (kyanite, wollastonite)

A

bladed

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19
Q

elongated with faces parallel to a common direction (apatite, beryl)

A

prismatic or columnar

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20
Q

easily split into sheets (muscovite, biotite)

A

foliated or micaceous

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21
Q

solid mass with no distinguishing features

A

massive

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22
Q

composed of many individual grains

A

granular

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23
Q

crystals emanating from a common point

A

radiating or divergent

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24
Q

composed of fibers

A

fibrous

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25
stalactite shaped
stalactitic
26
plates or slaps growing together
lamellar or tabular
27
contains aggregate of crystals giving a starlike appearance (pyrophyllite)
stellated
28
feathery appearance
plumose
29
like a branching tree or plant
dendritic or arborescent
30
net-like, lattice pattern
reticulated
31
spherical/hemispherical shapes made of radiating crystals
colloform or globular
32
similar to a bunch of grapes (hematite)
botryoidal
33
kidney-shaped
reniform
34
breast-like
mamillary
35
surfaces covered with fine crystals
drusy
36
small or small spheres
elliptic or pisolitic
37
mineral habit characterized by small, strong and flexible fibers.
asbestiform
38
commercial name for any marketable asbestiform mineral
asbestos
39
"white asbestos" is composed of what mineral? serpentine mineral group accounts for 95% commercial asbestos market
chrysotile
40
"blue asbestos" variety of riebeckite
crocidolite
41
"brown asbestos" variety of grunerite
amosite
42
when a mineral changes color as it is rotated to the polarizer in PPL
pleochroism
43
characterizes the relationship between the speed of light in a vacuum and the speed of light in that mineral
refractive index
44
refractive index of High mineral relief
> 0.12
45
refractive index of intermediate relief
0.04 - 0.12
46
refractive index of low relief
<0.04
47
relative refractive indices of two materials (minerals, glass, or epoxy) adjacent to each other in a thin section can be determined by using
Becke lines
48
if Becke line moves into the mineral grain the mineral has a _____ index of refraction and _____ relief
higher, higher
49
if Becke line move out of the grain, the mineral has a ____ index of refraction and _____ relief
lower, lower
50
ideal crystal form or the shape of a mineral takes when left to grow without barriers or interface with other nearby mineral grains
Mineral form
51
minerals show perfect or nearly perfect crystal faces
euhedral
52
minerals are rounded but still show general characteristic shape of that mineral
subhedral
53
crystals are completely irregular in shape and do not resemble the characteristic form for that mineral
anhedral
54
tendency of minerals to break along atomic planes of weakness within the crystal structure
cleavage
55
irregular cracks within a mineral
fractures
56
under XPL, the mineral will go extinct (dark) when the cleavage direction is PARALLEL to the N-S and E-W directions as the stage is rotated. what extinction is this?
parallel extinction
57
color of mineral under XPL is called
interference color
58
mineral separates into two minerals, producing a striped effect
exosolution lamellae
59
rocks in which clay content is predominant soft in nature and with the presence of water, they crumble easily if dry, crushed easily because of brittleness ex. shale, slate, laterite
argillaceous rocks
60
rocks in w/c calcium carbonate is the major ingredient generally hard but their durability is dependent on surrounding constituents ex. marble, limestone, dolomite
calcareous rocks
61
rocks contain silica in predominant amount presence of a large of free silica makes them harder and durable. strong resistance to weather ex. granite, chert, quartzite
siliceous rocks
62
twinning that has a planar composition surface separating two individual crystals. ex. orthoclase twinned on the Braveno law, with {021} as the twin plane
contact twins
63
twinning that has a planar composition surface separating two individual crystals. ex. crystal of orthoclase twinned on the Braveno law, with {021} as the twin plane
contact twins
64
twinning that have an irregular composition surface separting two individual crystals defined by a twin center or twin axis ex. crystal of orthoclase twinned on the Carlsbad Law with [001] as the twin axis
penetration twins
65
composition surfaces are parallel to one another ex. plagioclase, albite twin law with {010} as the twin plane
polysynthetic twin
66
composition surfaces are not parallel to one another ex. chrysoberyl along {031} plane
cyclical twins
67
feldspar minerals plagioclase and microcline are the most common that show twinning in this system
triclinic system
68
this system is most commonly occur on the plane {100} and {001} orthoclase and sanidine most commonly twinned both contact and penetration twins occur Maneback law {001}, contact twin Carlsbad Law [001], penetration twin Braveno Law {021}, contact twin Swallow Tail Twins {100}, gypsum
monoclinic system
69
commonly twin on planes parallel to a prism face {110} cyclical twins Staurolite Law
orthorhombic crystal (orthorhombic system)
70
twinning in this system usually occurs on {011} forming cyclical contact twins ex. rutile and cassiterite
tetragonal system
71
three types of twins common in isometric system
Spinel Law {111}, spinel [111] Iron cross [001], pyrite