chapter 7 metamorphism Flashcards
Thus, every metamorphic rock has a ______ —the rock from which it was formed
parent rock
_______________, which means to “change form,”
Metamorphism
Subducting sediments are metamorphosed due to __________________
increase in pressure and temperature
Shallow crustal rocks are metamorphosed by ____________
heat from rising magma
Deeply buried sedimentary strata are metamorphosed
burial metamorphism
forces that deform rock that are unequal in different directions and are referred to as ______________
differential stress
Pressure, like temperature, also increases with depth as the thickness of the overlying rock increases. Buried rocks are subjected to ____________, which is analogous to water pressure, in which the forces
are applied equally in all directions
confining pressure
When substantial chemical change accompanies metamorphism the process is called _____________
metasomatism
Recall that the term _______ is used to describe the size, shape, and arrangement of grains within a rock
texture
The term _________ refers to any planar (nearly flat) arrangement of mineral grains or structural features within a rock
foliation
__________ textures develop in a wide range of rock types and metamorphic environments when minerals in the parent rock recrystallize to form new minerals.
Porphyroblastic
Notice that the dark biotite crystals and light silicate minerals (quartz and feldspar) have separated, giving the rock a banded appearance called ________ texture.
gneissic
Under higher temperature- pressure regimes, the minute mica and chlorite crystals in slate begin to grow. When these platy minerals are large enough to be discernible with the unaided eye and exhibit a planar or layered structure, the rock is said to exhibit a type of foliation called ________
schistosity
_______ no preferred directional texture
non-foliated texture
Foliation can form in various ways, including:
-Rotation of platy and/or elongated minerals
-Recrystallization of minerals in the direction of preferred orientation
-Changing the shape of equidimensional grains into flattened or elongated shapes with preferred orientation