Lesson 6:Metamorphic Rocks Flashcards

1
Q

This happen due to the rock being in a condition different from
when it was formed – in most cases, this means higher temperatures
and pressures.

A

Metamorphism

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2
Q

This rock has the same over-all chemical composition as its parent rock* but may have different minerals and texture.

A

Metamorphic Rock

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3
Q

The rock before metamorphism happens.

A

Parent Rock

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4
Q

Metamorphic rocks are not normally considered as parent rock even though they can be metamorphosed. Only _________ rocks are considered as parent rocks

A

Igneous and Sedimentary

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5
Q

the parent rock of slate and schist

A

Mudstone

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6
Q

Controls what kind of metamorphism may take place.

A

Temperature

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7
Q

It is a function of temperature

A

Mineral stability

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8
Q

What factors causes a temperature change?

A

Pressure change and water availability

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9
Q

these are minerals that have the same composition as the mineral it crystallized from but different in crystal structure.

A

Polymorphs

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10
Q

Affects the texture of the resulting metamorphic rock.

It may also cause metamorphic rock’s foliation

A

Pressure

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11
Q

Facilitates ion transfer and may make metamorphic process go faster.

A

Water

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12
Q

Same pressure from all directions (pressure is also

applied in directions perpendicular to the page)

A

Equal confining pressure

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13
Q

Pressure from sides is higher than pressure at top and

bottom (pressure is also applied in directions perpendicular to the page)

A

Directed pressure

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14
Q

Pressure pushes one side in one direction and the other side in the opposite direction (like when your hands rub each other and the particle is
in between your palms)

A

Shear stress

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15
Q

A lot of _____ is needed for metamorphic process to happen

A

time

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16
Q

estimates of new mineral growths are around ____every million years.

A

1 mm

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17
Q

DIRECTED PRESSURE or SHEAR STRESS is needed in

the environment to form this kind of rock.

A

Foliated Metamorphic Rock

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18
Q

No directed pressure environment or

environment with little pressure (such as near surface)

A

Non-Foliated Metamorphic Rock

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19
Q

“layering” or “banding” in metamorphic rocks causing
“sheet-like” structure. Not necessarily seen as physical layers or bands always by the naked eye but show up as weakness planes of the rocks.

20
Q

These rocks do not show foliation even if they are formed in an environment with directed pressure

A

Quartzite and marble

21
Q

If a rock is squeezed (directed pressure), it may deform and texture will change such that the minerals seem _______ along an axis _______ to the bigger stress/squeeze.

A

elongated, perpendicular

22
Q

It can cause new minerals
to form and their growth will be along the axis perpendicular to the
direction of stress/squeeze.

23
Q

Factors contributing to foliation

A
  • Pressure (may include temperature change)

* Pressure, heat, and formation of new minerals

24
Q

biggest contributor of foliation.

A

Minerals growing and aligning to a certain direction(perpendicular to the biggest stress)

25
Foliated metamorphic rocks can be classified on
type of foliated texture it has , | grade of metamorphism
26
texture of slate rock
Slaty
27
texture of phyllite rock
Phyllitic
28
texture of Schist rock
Schistose
29
texture of Gneiss rock
Gneissic
30
From low-grade metamorphism of shale
slate rock
31
Property of slate rocks that causes it to break into flat sheets
Slaty cleavage
32
Slate rock's Microscopic clay and mica crystals have grown and aligned perpendicular to the
largest stress.
33
Similar to slate but heated to a higher temperature
Phyllite
34
Phyllite has larger mica crystals than in slate rocks but still barely visible to the eye as ________
sheen on the surface
35
Phyllite rocks form in ______layers
wavy / silky / crenulated
36
Created in high enough temperatures forming mica big enough to be seen by the naked eye, possibly with quartz, feldspar, etc. visible.
Schist
37
The temperature of schist is in between ____ and ____
Phyllite and Gneiss
38
its Minerals have been separated into distinct bands. | Little to no mica (temperature is too high for mica to remain)
Gneiss
39
Example of rocks that gneiss metamorphosised from
mudstone, sandstone, granite
40
Form in areas where pressure is just confining pressure (same pressure from all sides) or low-pressure conditions.
Non-foliatic metamorphic rocks
41
Non-foliatic metamorphic rocks are not _________ and the heat is coming from _________
buried deep enough, a nearby body of magma.
42
metamorphosed limestone
Marble
43
metamorphosed sandstone
Quartzite
44
metamorphosed fine grained rocks or volcanic rock
Hornfels
45
basalt at 150 degree celcius metamorphosis into
chlorite schist
46
• A rock that was partially melted and is metamorphosed – that is containing both igneous and metamorphic rock.
Migmatite