EXAM 2 MATERIAL Flashcards
when did petrography begin and who invented it?
- 1828
- william Nichol
How was petrography invented/developed?
Polarized light was produced from by cutting Iceland spar, a variety of calcite, into a prism.
what is the idea thickness of a thin section?
30 microns
what technique did henry Sorby develop?
-cutting rocks into thin slices, affixing them to a microscope so light could be transmitted through the crystal
what is a minerals’ refractive index?
how much the velocity of light slows when it passes through a crystal
how is refractive index calculated?
(the velocity of light in air)/(the velocity of light in the mineral)
how are refractive indices measured?
a device known as a refractometer
what is the angle of refraction?
the angle made by a refracted ray of light
define Snell’s law
sini/sinr=RI2/RI1
what is the angle of incidence
describes the angle light impinges on the boundary
what range of the electromagnetic spectrum is visible to the human eye?
400-700 microns
what is the velocity of light in a vacuum?
300,000 Km/s
is the speed of light the same in all materials?
NO, it slows thus resulting in the light ray bending (refraction)
what is retardation of light in minerals?
a function of the thickness of the mineral
what is the range and color of first-order interference colors?
red at 550 is first order interference color
0-550 nm
what is the range and color of second-order interference colors?
blue is second order interference color
550-1100 nm
what is the color of third-order interference colors?
pink
what is the nm range associated with each order color?
550 nm
Do isometric crystals exhibit interference colors, why or why not?
NO, crystals have three axes of equal length
what are isotropic materials?
have only one refractive index and are independent of the path of light
what is birefringence
the difference between the minimum and maximum index of refraction
why do interference colors exist
as the N-S fast and slow vibrating waves pass through the upper polarizer, they are out of phase, causing interference and their resulting colors.
what is extinction in minerals?
light is completely eliminated by the upper polarizer, appearing dark.
GO BACK TO ANISOTROPIC/ISOTROPIC SECTION (CH. 6)
are extinction angles important in mineral ID?
YES
what are fast and slow vibration directions related to?
promoninent crystallographic characteristics: cleavage, twinning
how can fast and slow vibration directions be measured?
with the use of an accessory plate
how is pleochroism observed?
in polarized light, the color of a mineral changes depending on the orientation of the crystal
what causes pleochroism?
the absorption of different wavelengths of light in different directions
is pleochroism a useful diagnostic property?
YES
what is the difference between a uniaxial and biaxial optical indicatrix
uniaxial has one optic axis biaxial two optic axes
which crystal classes have biaxial optical indicatrix and how many RI do they have?
- orthorhombic
- monoclinic
-triclinic
THREE RI
what are there two types of optical indicatrix?
- uniaxial
- biaxial
which crystal classes have uniaxial optical indicatrix and how many RI do they have?
- tetragonal
- hexagonal
TWO RI
what is the optic angle designated as?
2v
what is the optic angle measuring?
the acute angle between two axes
What is modal analysis
the areal abundance of a mineral
what techniques are involved in modal analysis?
comparing what is observed in thin section to a chart showing typical abundances
TERNARY diagram- CH7 slide 10
know how to solve and know how to normalize and plot lines on diagram
what percentage abundance must a mineral be to be considered major elements
more than 1 wt.%
what percentage abundance must a mineral be to be considered minor elements
1.0-0.1 wt%
what percentage abundance must a mineral be to be considered trace elements?
less than 0.1 wt%
what is the importance of silicon and oxygen in rock forming minerals?
the crust is made almost entirely of oxygen and silicates
BINARY DIAGRAMS- CH7 (slide 7)
calculation of mineral formulas
what is the difference and similarities between fayalite and forsterite as far as composition?
- both end members of olivine
- Fe rich= Fayalite
- Mg rich= forsterite
be familiar with the calculation steps in determining mineral formulas
ch 7 slide 8
what are tie lines and what do they represent?
horizontal lines connection two coexisting phases
how can igneous minerals be structured in a 3d manner
tectosilicates
what is the only SiO2 mineral that does not contain tectosilicates?
stishovite
what group has single chain silicates?
the pyroxene group
what group has double chain silicates?
the amphibole group
what are both chain structures known as?
inosilicates
what are sheet silicates known as?
phyllosilicates