Chapter 6: Metamorphism: Alteration of Rocks By Temperature and Pressure Flashcards
What is the parent rock of marble?
Limestone
What is the metamorphosed rock from limestone?
Marble
What is the parent rock of schist?
Shale
What is the metamorphosed rock from shale?
Schist
Exhume
To transport to the Earth’s surface
3 principal factors of metamorphism
Heat, pressure, fluid composition
Average rate that temp increases with depth in the crust
30 deg C/km
Geothermal gradient
The increase in temp with increasing depth in Earth’s interior
Geothermometer
A rock’s mineral composition, which determines the temperature at which the rock formed (because different minerals form at different temperatures).
2 plate tectonic mechanisms that form most metamorphic rocks
- subduction
* continent-continent collisions
2 kinds of pressure (stress) rocks are subjected to
- confining pressure
* directed pressure/differential stress
confining pressure
general force applied equally in all directions
directed pressure/differential stress
force exerted in a particular direction
Rate that pressure increases with depth in the crust
.3 to .4 kbars (kilobars) per km (300-400 bars/km)
geobarometers
Mineral assemblages that can be used as pressure gauges, to determine the pressure that the rock formed
metasomatism
A change in rock’s composition by fluid transport of chemical substances into or out of it
6 types of metamorphism
- regional
- contact
- seafloor
- high-pressure
- burial
- shock
regional metamorphism
- takes place where both high temps and pressures are imposed over large parts of the crust
- characteristic of convergent plate boundaries
- most widespread type
contact metamorphism
- heat from an igneous intrusion metamorphoses the rock immediately surrounding it, normally only affecting a thin zone of country rock
- heat is from intruding magma
- pressure only relevant where intrusion is at great depths
seafloor metamorphism
- associated with mid-ocean ridges
* hot lava heat sea water which circulates though the new ocean crust by convection; hot temperature alters the basalts
burial metamorphism
- affects a smaller amount of rock
- low-grade metamorphism caused by the progressive increase of pressure and temperature exerted by the growing layers of overlying sediments and rock
- begins at 6-10 km
high-pressure metamorphism
- pressures 8-12 kbars
- form at very low depths and take a long time to recycle to the surface
- most form in subduction zones as sediments scraped from oceanic crust and subducted to depths over 30 km
shock metamorphism
- occurs when a meteorite collides with Earth
* mass and velocity is transformed into heat and shock waves through the country rock
foliation
- a set of flat or wavy parallel cleavage planes produced by deformation of igneous and sedimentary rocks under directed pressure
- the most prominent textural feature of regionally metamorphosed rocks