Mineralogy Flashcards

1
Q

Mohs Scale, 1-10

A

Talc, gypsum, calcite, flourite, apatite, orthoclase, quartz, topaz, corrundum, diamond

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2
Q

Diaphaneity

A

Mineral transmits light

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3
Q

Asterism

A

Inclusions of tiny parallel slender fibers, refraction

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4
Q

Pleochroism

A

Different colors at different angles

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5
Q

Chatoyancy

A

Light reflection from luminous band

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6
Q

The law of the constancy of interfacial angles

A

The angles between the crystal faces of a given species are constant, whatever the lateral extension of these faces and the origin of the crystal, and are characteristic of that species.

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7
Q

Unit cell

A

The smallest subset of the lattice that still retains all of the physical, chemical, and symmetry properites of the mineral.

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8
Q

Isometric

A

The crystallographic axes used in this system are of equal length and are mutually perpendicular, occurring at right angles to one another.

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9
Q

Tetragonal

A

The tetragonal system also has three axes that all meet at 90º. C shortest

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10
Q

Orthorhomic

A

All three bases intersect at 90° angles, a=b X c

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11
Q

Hexagonal

A

The C or vertical axis is at 90º to the shorter axes, a X b X c. 90/90/120

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12
Q

Triclinic

A

In the triclinic system, all the axes are different lengths. None of them meet at 90º B/a/y

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13
Q

Quartz

A

SiO2 Hexagonal 1

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14
Q

Orthoclase

A

KAlSi3O8 Monoclinic 2

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15
Q

Albite

A

NaAlSi3O8 Monoclinic/Triclinic 3

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16
Q

Anorthite

A

CaAlSi3O8 Triclinic 4

17
Q

Muscovite

A

KAl2(AlSi3O10)(OH)2 Monoclinic 5

18
Q

Biotite

A

K(Mg,Fe)3(AlSi3O10)(OH)2 Monoclinic 6

19
Q

Amphibole

A

(Ca,Mg,Fe)7Si8O22)(OH)2 Monoclinic 7

20
Q

Pyroxene

A

(Ca,Mg,Fe)2Si2O4 Orthorhombic/Monoclinic 8

21
Q

Olivines

A

(Mg,Fe)2SiO4 Orthorhombic 9

22
Q

Calcite

A

CaCO3 Hexagonal 10

23
Q

Crust

A

Oxygen, Silicon, Aluminum

24
Q

Upper Mantle

A

Silicon, oxygen, magnesium, and iron. Olivines and pyroxenes

25
Q

Lower Mantle

A

Iron, magnesium, and silicates

26
Q

Outer Core

A

Iron and nickel

27
Q

Inner Core

A

Fe, Ni

28
Q

Radius Ratio, why care?

A

Radius ratio is the ratio of radius of the cation to the radius of the anion. We care because larger anions can have more cations, then determines the coordination.

29
Q

Orthopyroxene

A

Fe, Mg

30
Q

Clinopyroxene

A

Ca,

31
Q

Silicates are classified by

A

arrangement of silicate tetrahedra, Neo, Soro, Cyclo, Chain single and double, hydro, Phyllo, and Tecto

32
Q

Neosilicates

A

1:4 Si:O each tetrahedron is isolated