Silicates (ma'am mylene ver) Flashcards

1
Q

More than 2/3 of the Earth’s crust is composed of these minerals.

A

framework silicate minerals

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2
Q

A High-pressure, low-temperature polymorph of Quartz

A

Stishovite

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3
Q

A polymorph of Quartz exists in high to medium pressure and a wide variety of temperatures.

A

Coesite

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4
Q

A polymorph of Quartz exists in low temp and low pressure

A

Alpha-Quartz

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5
Q

A respiratory illness caused by inhaling unsafe levels of silica dust.

A

Silicosis

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6
Q

Uses of quartz

A

Raw materials for making glass
Semiconductor
Sealant
Abrasive/polish
Semiprecious stone (Jewelry)

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7
Q

violet or purple quartz

A

Amethyst

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8
Q

cause of the purple color of amethyst

A

due to the trace amount of Fe

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9
Q

pink or rose red variety of Quartz

A

Rose Quartz

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10
Q

cause of the pink or rose-red color of Quartz

A

uncertain but some rose quartz contains very fine inclusions of pink dumortierite

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11
Q

cause of the yellow color of the Quartz

A

fe content, irradiation, or some combination

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12
Q

yellow Quartz

A

Citrine

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13
Q

cause of the milky color of Quartz

A

abundant minute fluid inclusions

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14
Q

A red or brown microcrystalline variety of quartz

A

Jasper

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15
Q

A black or dark gray microcrystalline quartz

A

Flint

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16
Q

smoky brown of black quartz

A

Smoky quartz

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17
Q

cause of the smoky brown color of Quartz

A

produced by irradiation of quartz containing trace amounts of Al.

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18
Q

Most abundant minerals in the earth’s crust.

A

FELDSPAR GROUP

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19
Q

FELDSPAR GROUP is nearly found in what type of rock?

A

igneous rock

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20
Q

three principal compositional end members of the Feldspar group.

A

Alkali feldspars (K,Na)AlSi3O8/ K-feldspar (KAlSi3O8) (Orthoclase)
Albite (NaAlSi3O8)
Anorthite (CaAl2, Si2O8)

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21
Q

the 6 minerals in the plagioclase group

A

Albite An0- An10
Oligoclase An10-An30
Andesine An30-An50
Labradorite An50 – An70
Bytownite An70-An90
Anorthite An 90-An100

22
Q

Microcline

A

triclinic K-feldspar

23
Q

Orthoclase

A

monoclinic K-feldspar

24
Q

Low Sanidine

A

monoclinic K-feldspar

25
high Sanidine
monoclinic K-feldspar
26
K-feldspar produced by authigenic or low-temperature hydrothermal processes
Adularia
27
triclinic sodic alkali feldspar characterized by grid twinning
Anorthoclase
28
Similar to feldspars in both structure and physical properties but distinguishable chemically from feldspars by having less silica relative to the amount of Na and K.
FELDSPHATOIDS
29
Mineral under feldspathoids
Nepheline, Leucite Sodalite group
30
hydrated framework silicates
Zeolite Group
31
The largest single group of silicate minerals constitute major rock-forming minerals in some environments
Zeolite Group
32
produced by the alteration of some precursor minerals
Zeolite group
33
Environments favorable for minerals under the zeolite group
Weathering under high pH conditions Sedimentary diagenesis environments Alteration associated with percolating groundwater Hydrothermal alteration associated with igneous activity Contact metamorphism Burial and low-grade regional metamorphism
34
a mineral group that has a general formula of General Formula: XYZ2O6
Pyroxene group
35
Constructed of single chains of tetrahedra.
Pyroxene group
36
color of Orthopyroxenes and pigeonite
brown
37
usually restricted to volcanic rocks
pigeonite
38
Most of many members with platy or flaky habits and one prominent cleavage. They are generally soft, relatively low specific gravity
Phyllosilicates
39
chief minerals of schists and are widespread in igneous rocks
MIca
40
Form at lower temperatures than amphiboles or pyroxenes and frequently are formed as replacements of earlier minerals as a result of hydrothermal alteration
Phyllosilicates (sheet silicates)
41
which contain rings of linked SiO4 tetrahedra
Ring Silicates (cyclosilicates)
42
3 common species of ring silicates
Beryl Cordierite Tourmaline
43
Most abundant in the pyroxene group
Augite
44
Most common pyroxenes in igneous rocks (intermediate to mafic)
augite, pigeonite, and orthopyroxene
45
The mixture of enstatite and ferrosilite
Orthopyroxene
46
The mixture of diopside and hedenbergite
Clinopyroxene
47
generic term for the mixture of Mg2Si2O6 and Fe2Si2O6
Hypersthene
48
generic term for the mixture of CaMg2Si2O6 and ((Ca,Fe)2Si2O6)
Augite
49
In terms of abundance, these minerals are among the most common minerals, in basaltic and related rocks in the oceanic crust
pyroxene
50
very common minerals in wide variety of igneous and metamorphic rocks
Amphibole