CHPTR 7 Metamorphic Rocks Flashcards
protolith
parent rock
metamorphism
transformation of rocks as the result of heat, pressure, or fluid activities
- below melting point BUT higher pressure and temp. than lithification
lithostatic pressure
uniform stress/confining pressure
uniform field of pressure experienced by most rocks beneath Earth’s surface
directed pressure (differential stress
pushes mineral grains into one direction
geothermal gradient
25-30 degrees C
the rate at which the Earth’s temperature increases with depth
what can provide heat for the metamorphic process + how
burial increases temp. - the deeper you go, the hotter it is
volcanoes - heat from intrusions and lava flow heats underlying rocks
confining pressure + example
uniform stress in all direction - lithostatic stress
lithostatic stress
pressure experienced by rocks under the Earth’s surface
pressure due to 1km of rock
25 - 30 MPa
directed pressure
differential stress - pushes mineral grains into one direction
metastomatism
metamorphism due to fluid activity
how does fluid activity affect metamorphism
accelerate chemical change which can cause new minerals to form
origins of fluids that influence metamorphic activity (4)
- trapped in pore space in rocks
- released by magma
- dehydration reactions
- hydrothermal circulation
metamorphic processes (7)
- orientation of mineral grains
- recrystallization of existing minerals
- growth of new minerals
- segregation of minerals
- baking
- shearing
- partial melting
controlling factors in metamorphism
heat, pressure, fluids
index minerals for metamorphism grade
low to high
chlorite
muscovite
biotite
garnet / kyanite
staurolite
sillimanite
3 horrible index minerals for metamorphism
andalusite, quartz, feldspar
what do andalusite, kyanite and sillimanite have in common
polymorphs
what causes kyanite vs sillimanite
+ why don’t i care about andalusite
kyanite - high pressure
sillimanite - high temperature
andalusite is a bad index mineral
foliated texture
stripes - produced by the preferred orientation of platy minerals
non-foliated texture
do not exhibit preferred orientation of minerals
burial metamorphism
low temp, low pressure, just rocks underground
contact metamorphism
high temp, low pressure
near a magma chamber and the surface
aureoles
metamorphosed zones that surround plutons or other intrusions - its from contact metamorphism
how does distance from a pluton affect metamorphic grade
- high grade metamorphism close to pluton, low grade farther away
regional metamorphism
most common metamorphism
occurs during subduction or continent-continent collision
Barrovian metamorphism protolith
shale