AS metamorphic Flashcards

1
Q

Contact metamorphism

A

localised/smaller area

heat predominant diving force

takes place in rocks (country rock) intruded by magma

creates met areole

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2
Q

regional met

A

larger area 10-1000km2

predominant force = pressure

at C plate boundaries

likely foliation as pressure causes alignment

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3
Q

Dynamic met/ cataclasis

A

happens in fault zones

when rocks move fast each other quickly and suddenly

may be fairly old cold and brittle

crushed and ground into angular fragments and some recryst

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4
Q

foliation

A

texture found in met rocks formed by pref alignment of flat platy minerals e.g. clay

mid to high pressure and flat platy mins present to form

usually regional

unfoliated usually contact met and low pressure

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5
Q

foliated rocks and formation

A

all reg met and parent rock shale

slate- shale to slate

phyllite - slate to phyllite

schist- phyllite to schist

gneiss - schist to gneiss

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6
Q

Non foliated rocks and parents

A

Marble (contact or reg) - limestone to marble

Metaquartzite (contact or reg)-sandstone to meta

spotted rock (contact only)- shale to spotted

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7
Q

marble summary

A

parent- limestone

colour-white

texture- granoblastic ( same grain size, increases with grade)

min comp- calcite

type- contact or reg

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8
Q

metaquartzite summary

A

parent- quartz

colour-white/grey

texture- granoblastic ( same grain size, increases with grade)

min comp- quartz

type- contact or reg

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9
Q

spotted rock summary

A

parent- shale

colour-grey/purple/green or black

texture- fine grained, partly developed slatey cleavage

min comp- clay and micas

type- contact

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10
Q

slate summary

A

parent- shale

colour-grey/green/purple/black

texture- slatey cleavage

min comp- clay and muscovite and chlorite

type- low grade reg

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11
Q

Phyllite summary

A

parent- shale

colour-green/grey

texture- wavey foliation ,fine grain

min comp- clay and muscovite

type- low grade reg

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12
Q

schist summary

A

parent- shale

colour-silvery sheen

texture- schistosity, med grain

min comp- muscovite and biotite, quartz and GARNET

type- med reg

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13
Q

Gneiss summary

A

parent- shale

colour-light and black bands

texture- gneissose banding, coarse grained

min comp- biotite, feldspar, sillimanite and kyanite

type- high grade reg

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14
Q

index minerals

A

chlorite (low), muscovite and biotite, garnet (med), staurolite ,sillimanite and kyanite(high)

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15
Q

diagram of diff temps and pressures for diff grades

SEE IN BOOKLET

A

diagenesis- 200 (pressure) to 200 (temp)

not found on earth - 200-1000 pressure, 0-200 temp

contact met- 0-200 pressure and 200-800 temp

igneous- 200-1000 pressure and 600-1000 temp

low grade- up to 600 pressure and 300 temp

med grade- up to 900 pressure and 500 temp

high grade- 900 - +1000 pressure and 500-800 temp

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16
Q

metamorphic areole

A

igneous intrusions cause country rock to metamorphose and recrystalise due to heat

17
Q

George Barrow

A

first to recognise and map zones of progressive met

discovered met zonation in highlands (Barrovian zones)

in diff grades of met diff minerals found - index mins

Chlorite-biotite-garnet-staurolite-sillimanite-kyanite

18
Q

slatey cleavage

A

splits into thin sheets along cleavage planes
(fine low grade and must contain flat platy mins)

19
Q

schistosity

A

happens when alignment of flat platy minerals 90 degrees to max pressure

often find garnet porphyroblasts

20
Q

Gneissose banding

A

light and dark minerals separate into distinct bands

mica rich layer= foliated

pale layer = granoblastic

21
Q

porphyroblastic

A

larger crystals surrounded by smaller matrix

e.g. garnet mica schist

22
Q

granoblastic

A

unfoliated formed by heat, randomly orientated equidimensional crystals

23
Q

crenulation cleavage

A

2 or more stresses cause multiple foliations going against each other giving wavey appearance