Week 7 Flashcards

1
Q

Parent rock (protolith)

A

The rock before metamorphism

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2
Q

Metamorphic grade

A

The degree to which a parent rock changes during metamorphism. It varies from low grade (temperature and pressure) to high

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3
Q

Recrystallization

A

The formation of new mineral crystals in a rock that tend to be larger than the original

Change in shape and size of grains without changing ID of mineral

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4
Q

Noecrystallization

A

Brand new minerals formed from protolith

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5
Q

Confining pressure

A

Stress that is applied in all directions

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6
Q

Differential stress

A

Forces that are unequal in all directions

CONVERGENT PB

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7
Q

Compressional stress

A

Differential stress that shortens a rock body

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8
Q

Shear stress

A

J

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9
Q

3 types of stress

A

Differential
Compressional
Shear

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10
Q

Texture (foliation)

A

Refers to any planar( flat) arrangement of mineral grains or crystals within a rock. Driven by compressional stress. Includes banding/ cleavage

Layers

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11
Q

Non foliation

A

Tends to be one type. No layers

Where deformation is minimal
Hydrothermal

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12
Q

Contact metamorphism

A

Changes in rock caused by the heat from a nearby magma body

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13
Q

Hydrothermal metamorphism

A

Chemical alterations that occur as hot iron rich water circulates through fractures in rock

Enhances recrystallization

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14
Q

Subduction zone (burial) metamorphism

A

High pressure low temperatures metamorphism that occurs where sediments are carried to great depths by a subducting plate

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15
Q

Types of metamorphic environments

A

Hydrothermal: low pressure, low to mid temp

Contact: low pressure, low to high temp

Regional: low to high temperature and pressure

Subd zone; high pressure low temp

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16
Q

4 agents that drive metamorphism

A

Heat
Pressure
Directional stress
Chemically active fluids

17
Q

How is confining pressure different from differential stress

A

Confining pressure squeezes rock equally in all directions, differential is greater in one direction than others.

18
Q

Define foliation

A

Refers to any planar( flat) arrangement of mineral grains or crystals within a rock. Driven by compressional stress. Includes banding/ cleavage

19
Q

How does a slate change to a phylite and so on

A

Goes through regional metamorphism. Low to high grade metamorphism

Slate phylite schist gneiss

20
Q

What is the agent of hydrothermal metamorphism

A

Hot iron fluids / water

21
Q

What type of plate boundary is associated with regional metamorphism

A

Convergent plate boundary

22
Q

How does contact metamorphism work

A

Rocks surrounding a molten igneous body are baked. Alters rock adjacent to the heat source called an aureole.

23
Q

Regional metamorphism

A

Metamorphism associated with large scale mountain building

Folding and faulting

24
Q

Phase change

A

Transforms one mineral into another. Same composition different structure

25
Q

Metamorphic rocks

A

Meta= change from one rock type team another

Altering of any pre existing rock through a solid state Change

26
Q

Temperatures of metamorphism

A

200-700 degrees

27
Q

Causes of metamorphism 4

A

Heat- subducting lithosphere leads to recrystallization/ne

Pressure: confining/ differential stress. Leads to phase change/ neo

Water- hot water will accelerate processes

Importance of parent rock

28
Q

Is ductile high or low pressure?

A

(No fractures) high confining pressure

Fractures- low confining pressure

29
Q

Read figure 8.3

A

J

30
Q

Metamorphism

A

Transforms one rock type into another

Process that changes the mineralogy, texture, and sometimes chemical composition that of a rock