Chapter 7: Metamorphism: A Process of Change Flashcards

1
Q

What are metamorphic rocks?

A

Metamorphic rocks are those that have undergone solid-state alteration of preexisting rocks.
Meta = change. Morph = form

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2
Q

What are protoliths?

A

The preexisting rocks that are altered during metamorphism are called protoliths. Metamorphism can alter any protolith (igneous, sedimentary, or metamorphic)

  • pre-existing rock, irrespective of its origin or nature
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3
Q

Metamorphism occurs when the protolith is subjected (w/o melting) to:

A
  • Heat
  • Pressure
  • Differential stress (push, pull or shear)
  • Bathing in hydrothermal fluids
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4
Q

Where does metamorphism occur and at what temperature?

A

Metamorphism occurs between 250oC and 850oC and the depth to this temperature varies with tectonic setting.

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5
Q

What are the sources of heat?

A

Sources of heat: the geothermal gradient, magmatic intrusions, and tectonic compression

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6
Q

How can you tell if a rock is a metamorphic rock?

A

Metamorphic mineral grains are typically large and interlock with each other rather than being cemented.

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7
Q

What is foliation?

A

parallel alignment of platy minerals and/or the presence of alternating light- and dark-colored layers

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8
Q

Explain how heat causes metamorphism

A

heat causes the atoms to vibrate faster, stretching and bending chemical bonds. If bonds are stretched too far and break, they detach from their original neighbors, move slightly, and form new bonds with other atoms “recrystallization”

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9
Q

What is recrystallization?

A

a rearrangement of atoms within grains or the migration of atoms into and out of grains. Mineral grains grow larger at the expense of smaller ones until they interlock

  • modification of the shape and size of mineral grains without a change in the mineralogy.
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10
Q

Give an example to recrystallization?

A

Sandstone –> Quartzite
Limestone –> Marble
Snow flakes

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11
Q

How do minerals change size and shape?

A

Minerals change size and shape by dissolution and growth of crystals. The identity of the mineral does not necessarily change

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12
Q

Explain how pressure causes metamorphism

A

under the effect of pressure, mineral grains will deform depending on how fast and how the pressure is applied

As pressure increases, the space between mineral grains is eliminated as grains are pressed together. At higher pressures, grains dissolve where they contact and reprecipitate in the pore spaces forming larger grains. At even greater pressures, they may undergo a phase change to minerals that have a more compact atomic structure.

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13
Q

True/False

As pressure increases the density of the rock increases.

A

True

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14
Q

What is differential stress?

A

push, pull or shear

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15
Q

What is shear stress?

A
  • Shear stress moves part of a material sideways causing it to be smeared out. It is like sliding out a deck of cards.
  • Shear acts parallel to a surface
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16
Q

What is horizontal compression? Give an example

A

Compression is a common result of tectonic forces. Mountain building creates horizontal compression.

17
Q

True/False

The differential stress is applied equally in everywhere on the rock

A

False

pressure is not applied equally in all directions and the preferred orientation of minerals

18
Q

How are minerals oriented in case of differential stress?

A

Mineral grains orient themselves with their long axis perpendicular to the stress field

19
Q

______ is a metamorphosed conglomerate.

A

Metaconglomerate

20
Q

What is neocrystallization? Give an example

A

New minerals form from old. Protolith minerals become unstable and undergo chemical reactions that recycle elements to form a new mineral assemblage.

EX: clay and quartz –> quartz, garnet, mica

21
Q

The types of metamorphism and their settings:

  • Thermal—__________
  • Burial—____________
  • Dynamic—__________
  • Regional—___________
  • Hydrothermal—________
  • Subduction—__________
  • Shock—_________
A
  • Thermal—heating by a plutonic intrusion
  • Burial—deep burial in a basin
  • Dynamic—shearing in a fault zone.
  • Regional—P and T change due to orogenesis.
  • Hydrothermal—alteration by hot water leaching
  • Subduction—high-P and low-T alteration
  • Shock—extreme high P from a bolide impact.
22
Q

What kind of metamorphism happen by heating by a plutonic intrusion?

A

Thermal

23
Q

What kind of metamorphism happen by deep burial in a basin?

A

Burial

24
Q

What kind of metamorphism happen by shearing in a fault zone?

A

Dynamic

25
Q

What kind of metamorphism happen by P and T change due to orogenesis?

A

Regional

26
Q

What kind of metamorphism happen by alteration by hot water leaching?

A

Hydrothermal

27
Q

What kind of metamorphism happen by high-P and low-T alteration?

A

Subduction

28
Q

What kind of metamorphism happen by hock?

A

Shock

29
Q

What is metamorphic grade?

A

Metamorphic grade is a measure of the intensity of T and P conditions that lead to alteration. Different T and P conditions occur in different geologic settings.
Low grade—slight metamorphism
High grade—intense metamorphism

30
Q

What is metamorphic facies?

A

A metamorphic facies is a set of mineral assemblages that indicate a certain range of P and T conditions.
A given metamorphic facies includes several different kinds of rocks that differ from each other in terms of composition (i.e., mineral content) but all rocks of a given facies formed under roughly the same temperature and pressure condition