L11: Metamorphic Rock Flashcards

1
Q

What is metamorphism?

A
  • Occur when a rock is subjected to new temperatures and pressures
  • Rocks change mineralogically and texturally until its in equilibrium with the new set of temperatures and pressures
  • Changes the composition of a rock
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2
Q

What are the 3 types of metamorphism?

A
  • Contact
  • Burial
  • Regional
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3
Q

Contact metamorphism

A
  • Transformed by heat

- Hot magma rises to the surface

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4
Q

Burial metamorphism

A
  • Sediment is buried and accumulates under moderate temperatures and pressures
  • Follows on from diagenesis
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5
Q

Regional metamorphism

A
  • Buried deep into the crust, undergo elevated temperatures and pressures
  • Commonly takes place during mountain building and it occurs on scales much larger than simple intrusions
  • Think of subduction and mountain building!!
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6
Q

What do plate tectonics affect?

A

Greatly affects the metamorphic reactions because the process may move sediments and rocks from earth’s surface to interior, where the temperatures are higher

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7
Q

As you go ______, temperature goes ______.

A
  • Down

- Up

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8
Q

What is a geothermal gradient?

A
  • Increase in temperature with increasing depth
  • Steeper where crustal thinning occurs
  • Shallower where the continental lithosphere is old and thick
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9
Q

What do geologists use to study composition of rocks?

A

geothermometer/geobarometer

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10
Q

What is metasomatism?

A

Metamorphic process in which abundant fluids change the composition and texture of a rock

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11
Q

What are metamorphic textures?

A
  • Foliated
  • Granoblastic (non-foliated)
  • Porphyroblastic
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12
Q

Foliated rocks

A
  • Show alignment of minerals
  • Have preferred orientation due to directed stresses
  • Have clear texture
  • Typically slate, phyllite, schist, gneiss
  • Typical parent rocks = shale, sandstone
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13
Q

Granoblastic rocks (non-foliated)

A
  • No clear texture
  • Grow in equant shapes (such as cubes or spheres)
  • Form from metamorphism in which deformation is absent (such as contact metamorphism)
  • Hornfel, quartzite, marble
  • Parents: shale, basalt, limestone or dolomite
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14
Q

Porphyroblastic rocks

A
  • Large crystals set in a fine-grained matrix
  • Surrounded by much finer grain matric
  • Contact and regional metamorphism rocks
  • Dissolved and reorganized
  • Rock name: slate to gneiss
  • Parent: Shale
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15
Q

What else increases as the intensity of metamorphism does?

A

So does crystal size and coarseness of foliatio

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16
Q

Examples of non-foliated rocks

A
  • Marble
  • Quartzite
  • Hornfel
17
Q

Define metamorphic facies

A
  • The assemblage of minerals formed during metamorphism of a rock of a given composition subjected to a given temperature and pressure
  • Partly depends on the composition of the parent rock
18
Q

Zeolite minerals

A
  • A class of silicates that contain interstitial water in cavities within the crystal
  • AKA zeolite grade
  • Basalt usually lowest grain minerals
19
Q

Greenschists

A

A higher grade of metamorphosed rocks; abundant minerals include chlorite

20
Q

Amphibolites

A

Contain amphibole and then the granulites (often contain pyroxene)

21
Q

Blueschist

A
  • High pressure, moderate temperature

- Typically blue in color

22
Q

Ecologites

A

Produced in the highest temperature conditions

23
Q

What are the 2 essential points that characterize the concept of metamorphic facies?

A
  1. Different kinds of metamorphic rocks form from parent rocks of different composition at the same grade of metamorphism
  2. Different kinds of metamorphic rocks form at different grades of metamorphism from parent rocks of the same composition
24
Q

What are isograds?

A

Used to plot metamorphic grades over a regional metamorphic belt