crossed polarized light (XPL)
adding an additional polarizer called the analyzer to see different optical properties. this is generally on the top of the stage as a switch marked with an A
plane polarized light (PPL)
all microscopes have a polarizer below the stage on top of the light fixture, which only allows one direction of light to pass through
interference color
this is used to determine the birefringence of a mineral. in rotating the stage until it is furthest from extinction, at its brightest color. you choose the color near the center
birefringence
the property of some minerals that causes light to split into two rays when it passes through them. these typically show up in crystals that are hexagonal, tetragonal, and trigonal, which as uniaxial
pleochroism
some minerals will change color when the stage is rotated under PPL. it either is or isn’t and you always say what color it presents
relief
this is how distinct the mineral looks from the surroundings, and we generally look at the edges of a mineral to determine this
extinction
minerals that are not always black in XPL will typically go black every 90 degrees and we can measure the angles at which they go black.
opaque
metallic minerals are most often this. they will be solidly black in PPL or XPL.
interference figure
a figure observed with a conoscope when a section of a doubly refracting crystal is in the path traversed by convergent plane-polarized light
uniaxial
This will be a plus sign when observing the interference figure
biaxial
this will be curves at certain angles from 0 to 90 degrees when observing the interference figure
silicate
based on silicate tetrahedra (70-80% of our minerals). quartz SiO2- if there’s silicate in a mineral, it’s a silicate mineral
sulfate
sulfuric acid salts such as Barite and Gypsum
phosphate
phosphoric acid salts like Apatite
oxide
metal bonded to O2 like Cuprite
halide
contain halogen elements such as Cl, Br, F, I like Fluorite
carbonate
CO3 based like Calcite
native element
pure elements in solid form like Gold (Au)
tectosilicate
all SiO4 bonded to one another- Framework Silicates
phyllosilicate
basically Cyclo bonded together to form a flat regularly repeating structure (mica’s)
chain (ino-) silicate
a chain (single/double) of SiO4. each sharing two O with other tetrahedra- pryoxene or amphibole
nesosilicate
one SiO4 bonded to other elements
cyclosilicate
six SiO4 bonded in a ring form Si6O18
sorosilicate
two SiO4 bonded to form Si2O7 then bonded to other oxygen (sharing oxygen, which means one less)
how do we classify minerals based on composition
subclassify them based on the arrangement of tetrahedra relative to other elements
list common minerals for each subclassification of silicates
Nesosilicates: Forsterite, Fayalite, Kyanite/Andalusite/Sillimanite, Topaz. Sorosilicate’s: Epidote. Inosilicates (single-chain): pyroxenes (enstatite, ferrosilite, pigeonite, diopside, augite). Inosilicates (double-chain): amphiboles (hornblende, glaucophane). Cyclosilicates: Beryl, Tourmaline. Phyllosilicates: Talc, Illite, Chlorite, Biotite, Muscovite. Tectosilicates: Microcline, orthoclase, albite, andesine, labradorite, anorthite.
define plagioclase feldspar
two main endmembers: anorthite- Ca rich endmember (what moon is mostly made of), albite- Na rich endmember. Solid Solutions: Oligoclase, Andesine, Labradorite, Bytownite.
define alkali feldspar
Pure alkali polymorphs: orthoclase (monoclinic) and microcline (triclinic). mixed alkali with albite polymorphs: sanidine (monoclinic) and anorthoclase (triclinic). Unusual feldspars: celsian, hyalophane, buddingtonite.
define hydrolysis
the chemical breakdown of a compound and transformation of one mineral into another due to reaction with water
define ternary diagrams
we use a ternary diagram to talk about 3 component compositions
define QAPF diagram
we used a special stacked ternary diagram to talk about Igneous Rocks in particular. this is mostly for felsic and intermediate rocks. Q- quartz, A- alkali feldspar, P- plagioclase feldspar, F- feldspathoid
define biotite
microcline: tetra, sheet (brownish color)
define muscovite
define phlogopite
define kaolinite
define talc
define tetrahedra
define octahedra
define T-O-T
define T-O
define dioctahedral
define trioctahedral
define interlayer
explain the types of sheet silicate layer arrangements (T-O-T and T-O)
discuss the changes in physical properties based on layer arrangements
discuss the shrink swell ability of expanding clays and why it happens
define pyroxene
d
define amphibole
define pyroxenoid
define enstatite
define ferrosilite
define diopside
define augite
define actinolite
define tremolite
define cummingtonite
define glaucophane
differentiate between orthopyroxene, clinopyroxene, pyroxenoids, and amphiboles in thin section
d
what are the structural differences between pyroxenes, pyroxenoids, and amphiboles
define forsterite
define fayalite
define pryope
d
efine almandine
define kyanite
define sillimanite
define andalusite
define staurolite
explain how we identify different nesosilicates
discuss polymorphism of Kyanite/Sillimanite/Andalusite
how do you identify that a mineral is isotropic like garnet
these are minerals that are the same in all directions. in PPL they appear clear but in PPL they are always black
define beryl
describe why cyclosilicates are typically hexagonal crystal system
define calcite
define aragonite
de
define azurite
de
define malachite
explain differences between calcite and aragonite
discuss compositional similarities between minerals discussed so far in this course
define phosphate minerals
define apatite
define corundum
de
define rutile
define spinel
define brucite
define gibbsite
define bauxite
define geothite
why are hydroxide minerals softer than oxides?
describe where and how must hydroxides form
define/identify halogen
define fluroite
d
define halite
define sylvite
why are halide minerals often water soluble
where do most halide minerals form
define barite
define celestite
define gypsum board
discuss environments where sulfates are likely to form
define galena