Chapter 7: Metamorphism Flashcards

1
Q

Metamorphic rock

A

a rock that forms when a pre-existing rock, or protolith, undergoes a solid-state change in response to modification of its environment

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2
Q

What kind of change is meant in the context of metamorphism?

A

a metamorphic rock contains new minerals that did not occur in the protolith, and/or a new texture (arrangement of mineral grains) that differs from that of the protolith.

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3
Q

protolith

A

original unmetamorphosed rock

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4
Q

Metamorphic minerals

A

new minerals that grow in place within solid rock during metamorphism

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5
Q

metamorphic texture

A

defined by the arrangement of mineral grains, can be manifested by metamorphic foliation

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6
Q

processes that take place during metamorphism

A
  • recrystallization; shape and size of the crystals change without changing the identity of the mineral
  • phase change; changes one mineral into another
  • metamorphic reaction or neocrystallization; growth of new minerals that differ from those of the protolith
  • pressure solution: pressure of grains agains one another with water between them, grains dissolve, ions migrate away
  • plastic deformation; rock behaves like soft plastic so minerals can change shape without breaking
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7
Q

differential stress

A

when material undergoes squeezing or stretching unequally from different sides

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8
Q

preferred orientation

A

the alignment of grains within a rock

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9
Q

foliation

A

the parallel surfaces or layers that can occur in a metamorphic rock, can give the rock a striped or streaked appearance or it can give it the ability to split into thin sheets

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10
Q

examples of foliated metamorphic rocks

A
  • slate: metamorphism of shale or mudstone
  • phyllite: a fine grained rock with a silky sheen (phyllitic luster), white mica
  • schist: medium to course grain rock, defined by the preferred orientation of large mica flakes (muscovite or biotite), forms at higher temps than phyllite
  • gneiss: composed of alternating dark and light colored layers, dark are more mafic, light are more felsic
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11
Q

how do non-foliated metamorphic rocks occur?

A

either metamorphism occurred in the absence of compression or shear, or most of the new crystals are equant

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12
Q

examples of non-foliated metamorphic rocks

A
  • hornfels: a fine grained non-foliated rock which contains a variety of metamorphic minerals
  • quartzite: formed by metamorphism of pure quartz sandstone, looks glassier than sandstone and does not have the grainy, be a variety of colors
  • marble: metamorphism of limestone
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13
Q

metamorphic grades

A

indicates the intensity of metamorphism, meaning the amount or degree of metamorphic change. Depends on the temperature and pressure at which metamorphism takes place.

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14
Q

shearing

A

stretches the rock and flattens mafic components; smears rocks into parallel lines

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15
Q

protolith of quartzite

A

quartz sandstone

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16
Q

protolith of marble

A

limestone

17
Q

metamorphism of basalt from low grade to high grade

A

greenschist, amphibole, mafic granulite

18
Q

metamorphism of shale from low grade to high grade

A

slate, phyllite, schist, gneiss

19
Q

at an igneous pluton, where do the highest grade metamorphic rocks form?

A

In the wall rock of the pluton, also known as metamorphic aureole or contact aureole, the grade decreases further away from the pluton

20
Q

Since metamorphism in the wall rock of a pluton (contact aureole) takes place without application of differential compression or shear, what type of rock is formed?

A

hornfels

21
Q

dynamic metamorphism

A

occurs as a consequence of shearing under metamorphic conditions without requiring change in temperature or pressure, forms mylonite, occurs at plate boundaries, rifts, and collision zones

22
Q

dynamothermal metamorphism

A

involves heat and compression and shearing

- occurs beneath mountain ranges

23
Q

where is blueschist (blue colored amphibole) found?

A

only under accretionary prisms at subduction zones, forms as a result of compression and shearing

24
Q

shield

A

a broad region of long-lived, stable continental crust where sedimentary cover either was not deposited or has been eroded away so that precambrian basement rocks are exposed.