1. Minerals Flashcards
Why does temperature have a profound effect on metamorphism?
Temperature controls the stabilities of minerals and mineral assemblages
(Temp is more important than pressure)
Name and describe the three responses to heat
Recrystallisation
of existing minerals - changing texture
Neomineralisation
Formation of new minerals, due to chemical exchange between reacting minerals (no change in bulk comp except H2O and CO2)
Metasomatism
a special type of metamorphism involving reaction with infiltrating fluids (H2O plus dissolved species) -change in bulk composition
What is Stress?
Force per unit area, Pascal(Pa), bar, kbar
What is Load Pressure?
‘lithostatic pressure’ P, or confining pressure
acts uniformly in every direction
results from the weight of overlying rock
What is Deviatoric Stress
The part of the stress that is different in different directions
‘directed’ or ‘differential stress’
caused by lateral transmission of tectonic forces through the solid Earth’s crust
results in fracturing(faulting) in cold, brittle upper crust
results in plastic deformation in warm, ductile middle & lower crust
Describe the effects of heating due to intrusion of magma
contact metamorphism, in thermal aureoles around igneous intrusions
Usually no directed pressure, so foliation not developed
Describe regional metamorphism
heating, pressure increase and deformation
due to tectonic processes at convergent plate margins
- pressure increase due to burial
- temp increase due to geothermal gradient
- Deformation due to directed stress field
Describe dislocation(dynamic) metamorphism
deformation in fault zones
lithostatic pressure and temp not usually important
Describe shock metamorphism
Intense, short lived shock pressures due to meteorite impacts
Describe Slaty Cleavage
defined by aligned muscovites, oblique to bedding in a metamorphosed mudstone
Mudstones are composed mainly of:
- Detrital quartz
- Clay minerals (K,Mg,Al-rich silicates)
- Fe3+ oxides/hydroxides
Pelites contain:
- Quartz
- Micas and/or K-feldspar
- +-Al2SiO5 minerals, i.e. kyanite or sillimanite or andalusite
- (Fe,Mg) Al-Silicates e.g. garnet, chlorite, staurolite, cordierite, chloritoid