Chapter 8 - Metamorphism and Metamorphic Rocks Flashcards
Metamorphism
changes in mineral assemblage and texture that take place in rocks due to changes in temperature and/or pressure. These changes happen in a solid state
Chemical composition of original rock
determines mineral assemblage (most important factor)
Low grade
Low temperature and low pressure
high grade
high temperature and high pressure
stress
directed pressure
uniform stress
equal in all directions - creates igneous rocks - random alignment of materials
differential stress
unequal in all directions - creates metamorphic rocks - parallel alignment
intergranular fluid
acts as transporting medium and speeds up chemical reactions
vein
formed by precipitation of minerals from intergranular fluid into fracture
Prograde
rising temperature and pressure with water
Retrograde
falling temperature and pressure without water
Long periods of time
produce coarse grained rocks with high temperature and pressure
short periods of time
produce fine grained rocks with lower temperature and pressure and/or short reaction times
migmatite
composite rock - contains igneous and metamorphic components
foliation
planar texture - parallel mineral alignment due to differential stress