Optical and igneous Flashcards
(38 cards)
When light gets bent
Velocity changes
Rays get bent
2 new vibration directions
New colour
Pleochroism
Some anisotropic minerals strongly absorb light vibrating in one direction and transmit light vibrating in another
Extinction
When one of the vibration directions becomes parallel with the lower polarizer no light gets through the upper polarizer
Retardation
Amount by which the waves are out of phase
F= v/weird a thing
Frequency remains unchanged
If light speed changes weird a thing does
Weird a thing is related to colour and so if it changes colour also does
Uniaxial crystal structure
Hexagonal, trigonal, tetragonal
Biaxial crystal structure
Orthorhombic, triclinc, monoclinic
Retardation depends on
N of the two perpindicular vibration directions
Thickness of the crystal
Orientation of the crystal
Retardation is equal to
Thickness times nhigh- nlow
N is equal to
V air divided by v mineral
O Ray
Ordinary Ray
W
Vibrates perpindicular to the plane containing the optic axis
E Ray
Ray e
Vibrates in plane parallel to c axis
Mineral identification
Colour Relief Pleochroism Twinning: symmetric intergrowth of two or more crystals of the same mineral Cleavage: breaking of a mineral along crystallographically controlled planes Exosolution Alteration Zoning
Heat sources in the earth
- Heat from the early accretion and differentiation of the earth
- Heat released by the breakdown of unstable radioactive nuclides
Radiation
Transfer of Heat through particles/ waves through transparent material
Conduction
Transfer of kinetic energy from hot to cold in opaque minerals
Convection
Movement of ductile material due to density variations
Advection
Transfer of Heat with rocks that are moving
Classification criteria for igneous rocks
Colour: can be misleading
Texture: depends on cooling history so can be same
Minerals Present: depends on chemical comp
Chemical composition: most characteristic
Can vary
Need to be determined in lab
How does the mantle melt
Increase temp
Decrease pressure
Add volatiles
Partial melting
Separation of a partially melted liquid from the solid residue
Under what realistic circumstances can melts be created
Hot spots
Plates seperate: decompression melting
Fluid fluxing
Magmatic diversification
Partial melting
Magmatic differentation
Magmatic differentiation
Magma mixing
Mixed processes
Assimilation/contamination