FoG1 - Mineralogy Flashcards

1
Q

what structure has no bridging oxygens + net charge of 4- per cation

A

orthosilicate (isolated tetrahedra)

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
2
Q

example of orthosilicate

A

olivine, garnet, zircon

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
3
Q

what structure has one bridging oxygen per cation and a net charge of 2- per cation

A

chain silicate

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
4
Q

example of chain silicate

A

pyroxene

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
5
Q

how do chain silicates charge balance

A

layer 2 chain silicates with edge sharing octahedra layer in between (2+ cations)

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
6
Q

what structure has net charge on cation of 1.5- and 5/4 bridging oxygens

A

double chain silicate

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
7
Q

example of double chain silicate

A

amphibole

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
8
Q

Why can double chain silicates fit large cations in its structure

A

irregular octahedra leave large holes in structure

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
9
Q

how do double chain silicates charge balance

A

layer of octahedra between 2 double chain silicate layers

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
10
Q

what structure has 3/2 bridging oxygens and a net charge of 1- per cation

A

sheet silicate

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
11
Q

how do sheet silicates charge balance

A

have 2+ or 1+ cations in gaps in structure

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
12
Q

what structure has 4 bridging oxygens and a neutral charge per cation

A

3d framework

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
13
Q

example of 3d framework silicate

A

quartz

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
14
Q

example of sheet silicate

A

mica (biotite)

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
15
Q

what is the structure of feldspars

A

Al3+ replace Si4+ in framework structure, and additional cations fill gaps in structure, achieving charge neutrality

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
16
Q

what structure has 3 cations

A

triangular

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
17
Q

what structure has 4 cations

A

tetrahedra

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
18
Q

what structure has 6 cations

A

octahedral

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
19
Q

what structure has 8 cations

A

cubic

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
20
Q

what structure has 12 cations

A

cuboctohedral

21
Q

end members of olivine

A

forsterite = Mg
fayalite = Fe

22
Q

types of garnet

A

pyralspite series = have Al3+
ugrandite series = have Ca2+

23
Q

name 3 polymorphs pf aluminosilicate (Al2 SiO5)

A

kyanite
andalusite
sillimanite

24
Q

P-T of andalusite

25
P-T of sillimanite
high temp high pressure
26
P-T of kyanite
high pressure
27
why are zircons so good for dating
U4+ easily substitutes into crystal structure, but Pb2+ cannot. Therefore any Pb in the structure must have come from decay
28
solid solution for pyroxenes
Enstatite = Mg (SiO3) Ferrosilite = Fe (SiO3)
29
solid solution for pyroxenes with 50% Calcium
Diopside = CaMg (Si2O6) Hedenbergite = CaFe (Si2O6)
30
pyroxenes with ~50:50 Mg:Fe and varying Calcium
Pigeonite = some Ca Augite = less than 50% Ca
31
name of pyroxenes with <5% Ca
Orthopyroxene
32
name of pyroxene with 5-50% Ca
Clinopyroxene
33
general amphibole
Hornblende
34
physical characteristics of phyllosilicates
platy, layered, planar, layered structure flexible, soft as weak bonds between layers
35
what do most phyllosilicates have at centre of hexagons
-OH group (water)
36
2 ways of arranging octahedra in a sheet
tri-octahedral = all 3 sites occupied, 2+ cations di-octahedral = 2 / 3 sites occupied, 3+ cations
37
types of layering sheet silicates
1:1 = T-O 2:1 = T-O-T 2:1:1 = "T-O-T O T-O-T"
38
example of 1:1 layered sheet silicates
kaolinite (di-), serpentine(tri-)
39
example of 2:1 layered sheet silicate
chlorite group minerals
40
what goes between repeating 2:1 layered silicates
cations (K+) or cations and H2O
41
key phyllosilicates (clay minerals)
kaolinite muscovite serpentine
42
how are clays produced
weathering of anhydrous aluminosilicates
43
what reaction forms serpentine and what does it do
Forsterite + water -> serpentine + brucite serpentine lowers melting point of mantle at subduction zones
44
What are framework silicates
continuous network of conjoined Si tetrahedra, with all 4 O bonded to a neighbouring tetrahedra
45
phase transitions when heating quartz
low quartz -> high quartz -> tridymite -> cristobalite
46
high pressure polymorph of quartz
coesite
47
very high pressure polymorph of quartz created by impacts
stishovite
48
physical structure of low quartz (alpha)
trigonal, 3 fold symmetry