Chapter 7 Flashcards
metamorphism
processes of change that a rock undergoes when exposed to physical and chemical conditions significantly different from those that it formed from
metamorphic rock
end product of a rock that undergoes metamorphism
protholith
parent rock
texture of the protholith may change due to:
Recrystallization (when small grains of a mineral coalesce to form larger grains)
Pressure solution (if water is present, some minerals dissolve and the dissolved ions re-precipitate changing relationship between grains)
Alignment of grains (the result is foliation and lineation)
mineralogy of the protholith may change by
phase change: one polymorph changes to another more stable at the new conditions {there is no change in the chemical composition}
Neocrystallization: process of chemical reactions between protholith minerals during which ions from two or more minerals combine to create new minerals
diffusion
As temperatures rise, atoms vibrate more rapidly, and chemical bonds holding the atoms into the lattice of minerals begin to stretch and break, the freed atoms migrate slowly through the solid rock
Lithostatic pressure
results from the burial within the Earth and in all equal directions
lots of pressure at great depths
phase change
a new mineral with a more compact atomic arrangement can form that is more stable under the high-pressure conditions
polymorphs
minerals like diamond and graphite that have identical compositions but different internal structures
directed pressure
also called differential stress
type of pressure in a rock due to vise-like squeezing and or shear
phase diagram
has pressure and depth on the vertical axis and temperature on the horizontal axis
hydrothermal fluids
rocks that contain high-temperature liquids, gases, and ions of other elements have been dissolved
May be released from magma when the magma solidifies
metasomatism
when the chemical composition of a metamorphic rock changes significantly due to reaction with hydrothermal fluids
Contact metamorphism
occurs where rocks are subjected to elevated heat without a change in pressure and without the application of differential stress
happens when an igneous intrusion comes in contact with a rock
Regional metamorphism
occurs where rocks in a large region of crust are subjected to increases in temperature and pressure and differential stress
happens during mountain building