Metamorphic Pathways Flashcards
When rocks get covered up by thick layers of younger rocks, pressure and temperature rise
Burial metamorphism
Plate boundaries can increase P more than T. T more than P, or both to an extreme level
Tectonic Metamorphism
Burial metamorphism can happen…..
Anywhere
Contact, Burial, Regional, Subduction
Metamorphic Pathways
Temperature rises when rocks touch hot magma
Contant
Pressure rises when rocks go down a deep-sea trench
Subduction
Both P and T rise during continental collision
Burial –> Regional
Rock whose index minerals tell us the metamorphic pathway
Metamorphic Facies
Faces =
Clues to Tectonics
Ancient plate boundaries leave metamorphic rocks behind
long after the mountains erode.
Rock baked at low P to smooth porcelain texture by hot magma
Hornfels (contact zone facies)
Colored by high-pressure index mineral kyanite
Blueschist
Colored by moderate P/T index mineral chlorite
Green schist
When you see a greenschist zone parallel to a blueschist zone in a paired belt…
you know there was once a subduction zone there
Suture zone =
Very high P and T