shale
slate
phyllite
schist
gneiss
migmatite (partially melted)
new or different minerals appear
folliation appears
increased grain size
heat
pressure
fluids
deformation
size of intrusion
temperature of magma
fluid circulation
temperature difference btwn intrusion and host
composition of intrusion and host
speed of emplacement
fluid interactions (ground water and magmatic fluids)
shape of intrusion
chlorite
biotite
garnet
staurolite
kyanite
silimanite
k-feldspar
the grade changes in order from low to high temperature
more common since energy is more available
loss of volatiles occurs here
chlorite
epidote
amphibole
garnet
pyroxene
regional metamorphism
mid temp and pressure
mid to high pressure
low temp
low temp
low pressure
high pressure
mid to high temp
low pressure
mid to high temp
mid pressure
mid to high temp
mid to high pressure
high temperature