Chapter 7 Flashcards

1
Q

metamorphism

A

processes of change that a rock undergoes when exposed to physical and chemical conditions significantly different from those that it formed from

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2
Q

metamorphic rock

A

end product of a rock that undergoes metamorphism

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3
Q

protholith

A

parent rock

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4
Q

texture of the protholith may change due to:

A

Recrystallization (when small grains of a mineral coalesce to form larger grains)
Pressure solution (if water is present, some minerals dissolve and the dissolved ions re-precipitate changing relationship between grains)
Alignment of grains (the result is foliation and lineation)

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5
Q

mineralogy of the protholith may change by

A

phase change: one polymorph changes to another more stable at the new conditions {there is no change in the chemical composition}
Neocrystallization: process of chemical reactions between protholith minerals during which ions from two or more minerals combine to create new minerals

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6
Q

diffusion

A

As temperatures rise, atoms vibrate more rapidly, and chemical bonds holding the atoms into the lattice of minerals begin to stretch and break, the freed atoms migrate slowly through the solid rock

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7
Q

Lithostatic pressure

A

results from the burial within the Earth and in all equal directions
lots of pressure at great depths

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8
Q

phase change

A

a new mineral with a more compact atomic arrangement can form that is more stable under the high-pressure conditions

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9
Q

polymorphs

A

minerals like diamond and graphite that have identical compositions but different internal structures

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10
Q

directed pressure

A

also called differential stress

type of pressure in a rock due to vise-like squeezing and or shear

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11
Q

phase diagram

A

has pressure and depth on the vertical axis and temperature on the horizontal axis

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12
Q

hydrothermal fluids

A

rocks that contain high-temperature liquids, gases, and ions of other elements have been dissolved
May be released from magma when the magma solidifies

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13
Q

metasomatism

A

when the chemical composition of a metamorphic rock changes significantly due to reaction with hydrothermal fluids

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14
Q

Contact metamorphism

A

occurs where rocks are subjected to elevated heat without a change in pressure and without the application of differential stress
happens when an igneous intrusion comes in contact with a rock

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15
Q

Regional metamorphism

A

occurs where rocks in a large region of crust are subjected to increases in temperature and pressure and differential stress
happens during mountain building

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16
Q

Burial Metamorphism

A

happens when rocks are simply buries very deeply by overlying sediment

17
Q

Dynamic metamorphism

A

rock undergoes differential stress in response to shear along a fault zone but does not undergo a change in temp or lithostatic pressure

18
Q

Shock metamorphism

A

where a meteorite hits the Earth

enormous kinetic energy is converted to heat and differential stress

19
Q

Metasomatism

A

where hydrothermal fluids are present

20
Q

Classes of metamorphic rock

A
Aluminous
Quartzo-Feldspithic
Calcareous
Mafic
Organic
21
Q

preferred orientation

A

foliation and lineation

22
Q

foliation

A

if it contains a stack or parallel feature alternating bands of different material

23
Q

lineation

A

rod shaped minerals are aligned parallel to one another

24
Q

Slate

A

low grade metamorphosed shale or mudstone

25
Q

phyllite

A

a grade higher than slates

26
Q

schist

A

medium to high grade rock with a strong folitation

27
Q

Gneiss

A

high grade metamorphic rock of any composition minerals segregate into light and dark layers

28
Q

Anthracite coal

A

black shiny hard rock made of carbon that has no visible mineral grains and low specific gravity

29
Q

metamorphic grade

A

a broad, informal approximation of how much a rock has changed

30
Q

grain size

A

increases with increasing metamorphic grade

31
Q

porphyroblasts

A

minerals grow much larger than others in the rock
the larger the mineral the higher the metamorphic grade and the longer the rock stayed at its peak metamorphic temperature

32
Q

gnessic banding

A

compositional banding defined by alternating light and dark colored layers

33
Q

porphyroclasts

A

leftover grains of feldspar after the surrounding rock has changed into a mass of fine mica

34
Q

metamorphic index minerals

A

minerals that therefor indicate the conditions of metamorphism