Exam 2 Flashcards

(40 cards)

1
Q

What is the depth range for hypabyssal and plutonic rocks?

A

Hypabyssal: ~0-5 km; Plutonic: ~5+ km below the surface.

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2
Q

What mineral phases are part of mantle transition zones?

A

Wadsleyite and Ringwoodite

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3
Q

What is equilibrium crystallization

A

A process where crystals remain in contact with the melt during solidification.

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4
Q

What is fractional crystallization?

A

Crystals are removed from the melt as they form, preventing further reaction with it.

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5
Q

What are primitive magmas?

A

Magmas with very high liquidus temperatures and high MgO contents, such as picrite
basalt.

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6
Q

What are common types of mantle xenoliths?

A

Gabbroic, Dunite, Wehrlite, Lherzolite, Harzburgite, and Garnet-bearing peridotites.

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7
Q

What is the difference between aplite and obsidian?

A

Aplite is chemically similar to granite (dry), while obsidian is glassy and very hydrous.

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8
Q

What are the three main magma differentiation processes?

A
  1. Fractional crystallization
  2. Magma mixing
  3. Assimilation
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9
Q

What minerals indicate I-type vs. S-type granites?

A

I-type: Magnetite, hornblende;
S-type: Ilmenite, muscovite.

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10
Q

What causes deformation in metamorphic rocks?

A

Deviatoric stress-differential pressure causing stretching, compression, or shear.

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11
Q

What are primary metamorphic fluids

A

Fluid inclusions trapped during mineral formation, often in amphiboles, feldspar, or quartz.

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12
Q

What is an isograd?

A

A line on a geologic map indicating the first appearance of a particular metamorphic
mineral.

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13
Q

What minerals appear around 400-700°C in regional metamorphism?

A

400°C - Pyrophyllite;
420°C - Kyanite;
520°C - Chloritoid;
570°C - Staurolite;
630-690°C - Sillimanite.

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14
Q

What indicates high-grade metamorphism?

A

Presence of minerals like sillimanite, orthopyroxene, and spinel.

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15
Q

What are the three Al2SiO5 polymorphs and when do they form?

A

Kyanite (high pressure), Andalusite (low pressure), Sillimanite (high temperature).

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16
Q

What is the metamorphic significance of muscovite dehydration

A

Marks transition into high-grade conditions (e.g., amphibolite to granulite facies).

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17
Q

What is the solidus of water-saturated granite?

18
Q

What texture develops in high-grade metamorphic rocks?

A

Gneissic banding and schistosity due to mineral alignment under directed pressure

19
Q

Why does hornblende occupy a large area in the ACF diagram?

A

Due to its wide solid solution range.

20
Q

What minerals are common in greenschist facies?

A

Epidote, chlorite, and actinolite (noted for their green color).

21
Q

What happens to actinolite during the transition to blueschist facies?

A

It disappears, and blue amphiboles (e.g., glaucophane) appear.

22
Q

What is the purpose of the isothermal-isobaric graph?

A

It shows stable mineral assemblages under constant temperature and pressure conditions.

23
Q

What is metamorphic facies?

A

Ranges of pressure and temperature where characteristic mineral assemblages form.

24
Q

What minerals are typical in greenschist vs. eclogite facies?

A

Greenschist: chlorite, epidote, actinolite;
Eclogite: kyanite, garnet-rich, omphacite (pyroxene).

25
What is mélange and how does it form?
A chaotic mixture of rock types formed in subduction zones.
26
What are paired metamorphic belts?
Parallel belts showing contrasting metamorphic conditions (e.g., greenschist-blueschist) formed near subduction zones.
27
What setting leads to blueschist facies metamorphism?
Subduction zones with high pressure and low temperature.
28
very low temp facies
plag olivine pyroxene
29
3 arrow trajectories:
1. medium p/t: metamorphism barrovian sequence 2. low p/t: Buchan 3. high p/t: subduction
30
Low to high temperature
6: Albite epidote hornfels 7: low Pressure: low to high temp hornblende hornfels (hblt plag) 10: pyx hornfels (Plag+CPX+ OPX)
31
what is facies
facies are a group of minerals that form over certain ranges of p/t conditions
32
glaucophene
it only forms at low temp and high pressure and forms at subduction zones
33
Low P/T series
-contact metamorphism -hydrothermal metamorphism -1. hornfels(300*c-800*c) a.albite-epidote b.hornblende c. pyroxene
34
Medium P/T series
-orogenic events -greenschist facies (300-500) -amphibolite (500-700)
35
High P/T series
-subduction zones -blueschist facies (250) -eclogite (500) -granulite
36
amphibolite minerals
-hornblende -garnet -augite -plagioclase
37
granulite minerals
anhydrous -clinopyroxene -orthopyroxene -plagioclase -garnet
38
blueschist minerals
-glaucophene -blue amphibole -garnet -epidote -dragonite
39
ultra high pressure metamorphism
coesite and diamond
40
contact metamorphism
occurs when an igneous body intrudes into an area through fractures and bakes the adjacent rock