6 - Metamorphism and Metamorphic Rocks Flashcards

1
Q

rocks (igneous, sedimentary or metamorphic) that changed from its original form by extreme heat, pressure and fluid activity into an all-new form of rock

A

Metamorphic rocks

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2
Q

meta means…

A

change

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3
Q

morph means…

A

form

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4
Q

causes the minerals in the rock to become unstable so they either reorient themselves into layers, or recrystallize into larger crystals.

A

Metamorphism

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5
Q

Parent (SHALE)

A

Daughter (SLATE)

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6
Q

Parent (GRANITE)

A

Daughter (GNEISS)

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7
Q

Parent (QUARTZ)

A

Daughter (QUARTZITE)

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8
Q

Parent (Bituminous Coal)

A

Daughter (Anthracite)

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9
Q

Temperature increase with the depth of burial

Core of the earth is relatively warmer than the outer crust

A

Geothermal Gradient

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10
Q

uniform rock pressure, produces equal intensity of pressure from all directions.

A

Uniform (Lithostatic Pressure)

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11
Q

produces minerals grow in the line of resistance (perpendicular to the direction of maximum pressure) to cause banding within the rocks.

A

Directed Pressure

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12
Q

the process on which a rock’s chemistry changes as well as its assemblage

A

Metasomatism

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13
Q

the change in the shape of the rocks due to the force of stress, usually movement of a fault zone.

A

Strain

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14
Q

is the presence of mineral layers, which is an important feature for classifying mineral rocks.

A

Foliation

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15
Q

the most common process for the occurrence of metamorphic rocks. These rocks were typically exposed to tectonic forces and associated high temperatures and pressures ONLY.

A

REGIONAL METAMORPHISM or DYNAMOTHERMAL METAMORPHISM

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16
Q

the process by which the country rock that surrounds a hot magma intrusion is metamorphosed by the high heat flow coming from the intrusion.

A

CONTACT METAMORPHISM or THERMAL METAMORPHISM

17
Q

the zone of metamorphism that surrounds the intrusion.

A

Halo or Aureole

18
Q

the processes which affect rocks, usually involving water at lower temperatures and pressures than metamorphism

A

Rock Alteration

19
Q

commonly localized within a few meters of major faults or fractures, it may occur throughout zones a kilometer or more across.

A

Alteration

20
Q

is the breaking down of rocks which involves water and ice in the process.

A

Weathering

21
Q

caused by the effects of changing temperature on rocks, causing the rock to break apart. The process is sometimes assisted by water.

A

Physical weathering

22
Q

occurs when water continually seeps into cracks, freezes and expands, eventually breaking the rock apart.

A

Freeze-thaw

23
Q

occurs as cracks develop parallel to the land surface a consequence of the reduction in pressure during uplift and erosion.

A

Exfoliation

24
Q

caused by rain water reacting with the mineral grains in rocks to form new minerals (clays) and soluble salts.

A

Chemical weathering

25
Q
  • removal of rock in solution by acidic rainwater. In particular, limestone is weathered by rainwater containing dissolved CO2, (this process is sometimes called carbonation).
A

Solution

26
Q
  • the breakdown of rock by acidic water to produce clay and soluble salts.
A

Hydrolysis

27
Q
  • the breakdown of rock by oxygen and water, often giving iron-rich rocks a rusty-colored weathered surface.
A

Oxidation

28
Q

the weakening and subsequent disintegration of rock by plants, animals and microbes. Growing plant roots can exert stress or pressure on rock.

A

Biological/biotic weathering

29
Q

involves hot water rising from below, commonly from volcanic sources, this is the result of interaction of the rock with hot water fluids.

A

Hydrothermal alteration

30
Q

the chemical replacement of rocks by elements carried in the solution, due to introduction or removal of chemical constituents.

A

Metasomatism

31
Q

page or leaf-like

A

Folios

32
Q

No distinct layering character

Often a massive crystalline structure

Formed under uniform pressures

Formed around igneous intrusions where the temperatures are high but the pressures are relatively low and equal in all directions (confining pressure)

A

Non-foliated metamorphic rocks

33
Q

Rock has distinct banding or layering, often not smooth like in sedimentary rocks

A

Foliated metamorphic rocks