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
- removal of rock in solution by acidic rainwater. In particular, limestone is weathered by rainwater containing dissolved CO2, (this process is sometimes called carbonation).
Solution
26
- the breakdown of rock by acidic water to produce clay and soluble salts. 
Hydrolysis
27
- the breakdown of rock by oxygen and water, often giving iron-rich rocks a rusty-colored weathered surface.
Oxidation
28
the weakening and subsequent disintegration of rock by plants, animals and microbes. Growing plant roots can exert stress or pressure on rock.
Biological/biotic weathering
29
involves hot water rising from below, commonly from volcanic sources, this is the result of interaction of the rock with hot water fluids.
Hydrothermal alteration
30
the chemical replacement of rocks by elements carried in the solution, due to introduction or removal of chemical constituents.
Metasomatism
31
page or leaf-like
Folios
32
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)
Non-foliated metamorphic rocks
33
Rock has distinct banding or layering, often not smooth like in sedimentary rocks
Foliated metamorphic rocks