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Pyroxene vs Amphibole
amphibole is long rectangles
pyroxene is samller cubic shape
Micas
Shiny like silicate minerals
Biotite = black shiny
Muscovite = white shiny
Regional Metamorphism
Foliated, high pressure and moderate heat
plate collisions
Contact metamorphism
non-foliated, high temperature and low pressure
back arc area of subduction zones (magma intrusions)
magma is hot and causes contact metamorphism around rocks
dominant rock is hornfels
nonfoliated rocks
contact metamorphism
High Temperature
Hornfelsc, Marble, Quartzite, Skarn
foliated rocks
regional metamorphism
high pressure, temperature, stress
Slate, Phyllite, Schists, Gneiss
Slate
dense and compacted
very flat
low-temperature metamorphism
phyllite
low-medium temperature
satiny luster (fish scales) - muscovite
garnet is often found
schist
medium-high grade metamorphism
schistosity - parallel alignment of large mica crystals
can identify w naked eye
gneiss
highest metamorphic grade
clearly defined white and black banded foliation (very obvious)
increases temperature causes melting, so half or some rock is melted and the bands are contorted