EOS 316 Midterm 1 Flashcards

1
Q

Where are igneous rocks sourced from?

A

Mantle-derived melts

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2
Q

How does the mantle melt? (3 ways)

A

(1) Increasing temperature
(2) Lower the pressure (adiabatic rise)
(3) Add volatiles (H2O)

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3
Q

What are the characteristics of the ocean crust (thickness, composition)?

A

10km thick, uniform stratigraphy, mafic, ophiolite suite top down (sediments, pillow basalt, sheeted dikes, massive gabbro)

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4
Q

What are the characteristics of the CC (thickness, composition)

A

~35km thick, highly variable composition (average: granodiorite), buoyant - unsubductable

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5
Q

Describe the composition and rheology of the mantle

A

ultramafic, mainly solid, viscous

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6
Q

Describe the composition and rheology of the earth’s core

A

Fe-Ni metallic alloy, outer core liquid, inner core solid

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7
Q

describe the pressure gradient as we move deeper inside the earth

A

Pressure increases linearly through the mantle (~1kbar every 3 km), increases more rapidly inside the core since the alloy is more dense

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8
Q

How does temperature change as we move deeper inside the earth?

A

-Thermal energy dominantly comes from the decay of radioactive elements in the mantle

-The lithosphere geotherm is approximately ~25ºC/km

-Mantle: small dT/dz - stays hot!
Lithosphere: Large dT/dz - temp drops fast!

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9
Q

how does the mantle melt to produce magmas at (a) divergent boundaries, (b) convergent boundaries, (c) hotspots?

A

a) decompression melting
b) flux melting
c) decompression melting

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10
Q

How do we classify igneous rocks? (3)

A

(1) Texturally: grain, crystallinity
(2) Modally: naming an igneous sock based on the percentage of each mineral present
(3) Chemically

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11
Q

What’s the difference between holocrystalline, hypo crystalline, and holohyaline?

A

holocrystalline: all crystal
hypocrystalline: part crystal, part glass
holohyaline: all glass

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12
Q

What is a porphyritic / phyric rock texture?

A

visibly large crystals in a finer-grained groundmass.

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13
Q

how-to QAP

A

(1) Analyze all minerals within the rock
(2) Normalize out any non-QAP (mafic / ultramafic)
(3) use new QAP minerals for analysis and name using chart

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14
Q

how-to non-QAP

A

(1) Analyze all minerals within the rock
(2) Normalize out any QAP (felsics)
(3) use new QAP minerals for analysis and naming scheme

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15
Q

When is normative mineralogy useful?

A

a) fine-grained, extrusive rocks: ~hypothetical mineral assemblage
b) helps distinguish between magma types

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16
Q

What are the types of silica saturation from normative minerals - Si:(Fe + Mg) ? (ratio and name)

A

(1) Quartz 1:n/a - ‘Si-oversaturated’
(2) Opx (hypersthene): 1:1 ‘Si-saturated’
(3) Olivine: 1:2 ‘Si-undersaturated’

17
Q

What are Si-saturated rocks?

A

(1) Normative hypersthene, normative olivine
(2) no quartz, no feldspathoids

18
Q

What are the types of silica saturation from normative minerals - Si:(Na + K) ? (ratio and name)

A

(1) Quartz
(2) Feldspathoids
(2a) Leucite: KAlSi2O6
(2b) Nepheline: (Na,K)AlSiO4

19
Q

What are Si-oversaturated rocks?

A

(1) Normative quartz, normative hypersthene
(2) No feldspathoids, no olivine

20
Q

What are Si-undersaturated rocks?

A

(1) Normative feldspathoids, normative olivine
(2) No quartz, no hypersthene

21
Q

How can we subdivide rocks in the alkaline field? (3)

A

(1) Hi-K series
(2) K-Series
(3) Na-Series

22
Q

How can we subdivide rocks in the sub alkaline field? (2)

A

Tholeiitic series
Calc-alkaline series

23
Q

At what setting can you find alkaline magmas?

A

Convergent plate margins, oceanic plates, continental plates

24
Q

At what setting do you find tholeiitic magmas?

A

Convergent plate margins, divergent plate margins, oceanic plates, continental plates

25
Q

Ate what setting can you find calc-alkaline magmas?

A

convergent plate margins

26
Q

What components are (/can be) in a magma? (4)

A

(A) melt (liquid)
(B) Crystals (solid)
(C) Volatiles (fluid = dissolved or exsolved gas)
(D) Possibly xenoliths or xenocrysts

27
Q

Describe the melt of a magma

A

-linked silica tetrahedra
-can have non-binded oxygen making it impure

28
Q

How do NBO’s affect the melt of a magma?

A

more NBO’s = depolymerized melt
less NBO’s = more H2O can dissolve

29
Q

What are the most important volatiles in a magma (2)?

A

(1) H2O
(2) Sulphur

30
Q

What controls magma behaviour? (4)

A

(1) Viscosity / composition
(2) Temperature
(3) Density
(4) Exsolution of dissolved volatiles

31
Q

What variables affect viscosity? (4)

A

(1) composition (wt% SiO2)
(2) Temperature
(3) % Crystals
(4) % Dissolved volatiles (eg. H2O)

32
Q

What is the top –> down order for an ophiolite sequence?

A

Pelagic sediments –> pillow basalts –> sheeted dikes –> gabbros

33
Q

How do hydrothermal fluids interact with ocean magma?( 4)

A

(1) Hot upwelling fluids reacting with rock
(2) Hydrothermal metamorphism
(3) Some areas concentrate large volumes of upwelling fluids
(4) Metasomatism = rock changes compositionally and mineralogically via fluids

34
Q

What is a phase?

A

A physically distinct, mechanically separable phase (liquid, solid, gas)