Crystal Geochemistry Flashcards

1
Q

What are the states of matter?

A

Solid, liquid, gas

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2
Q

Three factors controlling crystal structures

A

1) Size of ions
2) Valences of ions
3) Bonding between atoms

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3
Q

Coordination number

A

The number of anions that surround a particular cation in an ionic crystal

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4
Q

Does the coordination number increase or decrease as the radii of anions and cations get closer?

A

Increase

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5
Q

True or False: The size of an ion is influenced by the coordination number.

A

True

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6
Q

Ionic substitution in crystals

A

Some of the ions of the major elements may be substituted by other minor/trace elements (not 100% pure)

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7
Q

Why does a mineral that is composed of limited number of major elements contain so many trace elements?

A

Because most minerals are not composed purely of the major elements. So, they need minor/trace elements to substitute.

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8
Q

Goldschmidt Rule #1

A

The ions of one element can replace those of another in crystals if their radii differ by less than about 15%

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9
Q

Goldschmidt Rule #2

A

Ions whose charges differ by one unit substitute readily for one another provided electrical neutrality is maintained.

If charges differ by more than one, substitution is generally slight.

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10
Q

Goldschmidt Rule #3

A

When two different ions occupy a crystal lattice, the ion with higher ionic potential forms a stronger bond with the anions surrounding the site

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11
Q

Goldschmidt Rule #4 (Ringwood’s rule)

A

When the competing ions have different electronegativities and form bonds of different ionic character

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12
Q

Camouflage

A

Substitution by a minor element when they have the same charge and similar radii

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13
Q

Capture

A

Substitution by a minor element because the latter has a higher ionic potential

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14
Q

Admission

A

Substitution by a minor element when the latter has a lower ionic potential (larger radii / lower charge)

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15
Q

Coupled Substitution

A

When an ion is substituted by an ion of higher charge, another position must be occupied by one with a lower charge. Goal = electrical neutrality

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16
Q

Incompatible elements

A

Trace elements that cannot find crystals to accommodate them. So they remain the melt of a magma system

17
Q

Distribution coefficient

A

Concentration of an element in the crystal vs that in the melt

18
Q

Compatible elements

A

Elements that can be accommodated by the Fe-Mg-Ca minerals

19
Q

Typical compatible elements

A

Mn, V, Co, Ni, Cr

20
Q

Lanthanide contraction

A

Decrease of radii of REE ions with increasing atomic number

21
Q

What does the REE pattern reflect?

A

The degree of enrichment of different REEs

22
Q

Eu anomaly

A

Abrupt change of Eu compared to neighbouring elements in the REE pattern

23
Q

What mineral is “U” compatible with?

A

Zircon

24
Q

The more positive the anomaly, the more _____

A

oxidizing

25
Q

The more negative the anomaly, the more _____

A

reducing

26
Q

Mineral geothermometer

A

Tool that measures the temperature in a mineral. The higher the T, the easier the substitution.

27
Q

Two examples of a mineral geothermometer

A

1) Sphalerite geothermometer
2) Arsenopyrite geothermometer

28
Q

Why is U concentrated in granitic rocks, while Cr in ultramafic rocks?

A

Most granitic rocks result from evolved magma… U is incompatible, so it will stay in the melt and become enriched in granite.
Cr is taken away early in crystallization = mafics

29
Q

How can the concentrations of trace elements in minerals be used to estimate the formation temperature of the minerals?

A

Geothermometers. The higher the temperature, the higher the substituion.