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
Slaty Cleavage
fine grained rock splits into plate like fragments along planes - low grade - new mineral grains can only be seen with microscope
Schistosity
parallel but not necessarily planar arrangement of minerals - high grade - grains can be seen with unaided eye
Marble
metamorphic limestone or sandstone
Metamorphism of shale and mudstone
Slate (low grade) - phyllite (intermediate grade) - Schist (high grade) - Gneiss (high grade)
Quartzite
forms from quartz sandstone
Mechanical deformation
high pressure - physical transformation
chemical recrystallization
high temperature - change in crystallization
Cataclastic metamorphism
uncommon - mechanical deformation with minor chemical recrystallization - elongated grains fragments - foliated
contact metamorphism
uncommon - chemical recrystallization with minor mechanical deformation - occurs adjacent to hot magma bodies
metamorphic aureole
well defined shell of altered rock adjacent to intrusion (halo)
Hornfels
hard, fine grained rock that is formed by contact with small intrusion without fluid
Regional metamorphism
most common and widespread - (differential stress) mechanical deformation and chemical recrystallization - distinctly foliated