Optical and igneous Flashcards

(38 cards)

0
Q

When light gets bent

A

Velocity changes
Rays get bent
2 new vibration directions
New colour

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1
Q

Pleochroism

A

Some anisotropic minerals strongly absorb light vibrating in one direction and transmit light vibrating in another

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2
Q

Extinction

A

When one of the vibration directions becomes parallel with the lower polarizer no light gets through the upper polarizer

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3
Q

Retardation

A

Amount by which the waves are out of phase

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4
Q

F= v/weird a thing

A

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

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5
Q

Uniaxial crystal structure

A

Hexagonal, trigonal, tetragonal

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6
Q

Biaxial crystal structure

A

Orthorhombic, triclinc, monoclinic

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7
Q

Retardation depends on

A

N of the two perpindicular vibration directions
Thickness of the crystal
Orientation of the crystal

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8
Q

Retardation is equal to

A

Thickness times nhigh- nlow

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9
Q

N is equal to

A

V air divided by v mineral

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10
Q

O Ray

A

Ordinary Ray
W
Vibrates perpindicular to the plane containing the optic axis

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11
Q

E Ray

A

Ray e

Vibrates in plane parallel to c axis

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12
Q

Mineral identification

A
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
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13
Q

Heat sources in the earth

A
  1. Heat from the early accretion and differentiation of the earth
  2. Heat released by the breakdown of unstable radioactive nuclides
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14
Q

Radiation

A

Transfer of Heat through particles/ waves through transparent material

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15
Q

Conduction

A

Transfer of kinetic energy from hot to cold in opaque minerals

16
Q

Convection

A

Movement of ductile material due to density variations

17
Q

Advection

A

Transfer of Heat with rocks that are moving

18
Q

Classification criteria for igneous rocks

A

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

19
Q

How does the mantle melt

A

Increase temp
Decrease pressure
Add volatiles

20
Q

Partial melting

A

Separation of a partially melted liquid from the solid residue

21
Q

Under what realistic circumstances can melts be created

A

Hot spots
Plates seperate: decompression melting
Fluid fluxing

22
Q

Magmatic diversification

A

Partial melting

Magmatic differentation

23
Q

Magmatic differentiation

A

Magma mixing
Mixed processes
Assimilation/contamination

24
Two essential processes of magmatic differentation
1. Creates a compositional difference between one or more phases in response to a change in a variable like pressure temperature of composition 2. Preserves a chemical difference by segregating a chemically distinct portion so that they may either form a rock or continue to evolve as seperate systems
25
Effective ness of magmatic differentation depends on
Contrasts in physical properties such as density viscosity and diffusivity
26
Equilibrium crystallization
Implies a mass balance; overall composition remains constant throughout crystallization
27
Fractional crystallization
Implies that all crystallizing solids are removed or seperated from the magma as they form
28
Assimilation
Wall rock must first be partially melted and the heat has to come from the magma itself
29
Magma properties
Viscosity Temperature Composition Density
30
Viscosity depends on
Density Volatile content Temperature
31
Eruptive violence depends on
1. Amount of gas | 2. Ease with which gas escapes
32
Chlorite zone
Chlorite, muscovite, quartz, albite | Greenschist facies
33
Biotite zone
Biotite, muscovite, quartz, albite | Greenschist facies
34
Garnet zone
Garnet, biotite, quartz, muscovite | Amphibolite facies
35
Staurolite zone
Staurolite, garnet, biotite, quartz | Amphibolite facies
36
Kyanite zone
Kyanite, garnet, biotite, quartz | Amphibolite facies
37
Silimanite zone
Sillimanite, quartz, garnet, biotite | Amphibolite- granulite facies