Lecture 5 Flashcards

1
Q

The most abundant chemical elements in the continental crust

A

Dominantly oxygen and silicon

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2
Q

Differentiation process causes _____ elements to sink to the core, while _____ elements such as ________ and _______ , stay near the crust

A

Heavier
Lighter
Oxygen and silicon

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3
Q

First column of periodic table

A

Form bonds with silicon so enhanced concentration of these elements found at the crust

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4
Q

Radiogenic isotopes

A
  • radioactive and decay at known rates
  • unstable
  • used for radiometric dating
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5
Q

Radiogenic coupling example

A

87Rb (unstable) to 87 Sr (stable)

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6
Q

By 1 half life the parent and daughter atoms are

A

50:50

Have equal concentrations

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7
Q

What time of bonding is found in most minerals

A

Ionic bonding

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8
Q

Structure of diamond versus structure of graphite

A
  • both covalent bonding
  • diamond has strong bonds whereas graphite (forms sheet bonds) which are weaker
  • same chemical composition; only differ in their framework
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9
Q

Bonding in solids typically produces a __________

A

Crystal lattice

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10
Q

Definition of a crystal

A

Regular arrangement of atoms (crystal lattice)

This arrangement is responsible for many mineral properties

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11
Q

Minerals are a __________ of crystals

A

Subset

All minerals are crystals but not all crystals are minerals

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12
Q

Four criteria for a crystal to be called a mineral

A
  1. Naturally occurring
  2. Solid
  3. Specific chemical composition or range of compositions (I.e.., constant composition that can’t change into something else)
  4. Repeating atomic configuration-crystal structure or crystalline
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13
Q

A rock is

A

A mixture of minerals

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14
Q

Most common type of mineral in Earth’s crust

A
  • silicate anion or the tetrahedron (SiO4)4-

- combination of Si4+ with 4 O2-

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15
Q

Minor minerals

A
Oxides
Carbonates
Sulfides
Native elements
Sulphates
Phosphates
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16
Q

The silicate anions can be found as

A

Isolated tetrahedra

Polymerize into pairs, rings, sheets, chains, or frameworks

17
Q

Isolated tetrahedra

A
  • single tetrahedron
  • olivine (Mg2SiO4)
  • cleavage: none

Held together by ionic bonds

18
Q

Single chain silicate

A
  • single chain
  • pyroxene group CaMg(SiO4)2 (variety: diopside)
  • cleavage: two directions at 90 degrees
19
Q

Double chain silicates

A
  • double chain
  • Amphibole group Ca2Mg5(Si4O11)2(OH)2 (variety: tremolite)
  • cleavage: two directions at 120 degrees
20
Q

Sheet silicates

A
  • Mica
  • forms a sheets
  • cleavage: one direction
21
Q

Framework silicates

A

Feldspar:

  • 3D network
  • cleavage: two directions at 90 degrees

Quartz:

  • undisturbed pure network
  • cleavage: none
22
Q

What are the most abundant minerals in the continental crust

A

Silicates (95% of all minerals in the crust)

23
Q

Mineralogy of Earth’s mantle

A

Upper: dominantly silicates

Lower: silicates and oxides

24
Q

What are the most common types of silicates in the earth’s crust

A

Feldspar at 60%

Quartz at 15%

Reminding 20% are other forms of silicates (5% non silicates)