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elements
92 naturally occurring
8 common in earths crust
which 2 elements are most common
oxygen and silicon
most common minerals are made of…
oxygen, silicon, and a few other elements
native elements
composed of a single element
gold, silver, copper, sulphur
carbon occurs as diamond
mineral groups are classified by…
negative anion or radical
sulfides
sulfide minerals found in many types of rock
sulfur + metallic element
economically important!
oxides- Magnetite (Fe3O4)
aka lodestone
spontaneously magnetized
loses magnetism above Curie temp. (858K)
historically used in compasses
oxides- Haemetite (Fe2O3)
not spont. magnetized
major source of iron ore
characteristically green + brown/red
oxides- alumina corundum (Al2O3)
most common crystalline form
contains traces of Ti, Fe, Cr
impurities determine colour!
second hardest mineral after diamond
oxides- uranite
aka pitchblende
radioactive
Athabasca Basin (sask) = major producer
halides
anion is a halogen
ex. Halite (NaCl)
ex. Sylvite (KCl)
silicates
anion is silica tetrahedra: (SiO4)^4-
covalent bond between Si and O
electric charge balanced by cations between the silica tetrahedra
how are silicate metals classified
geometry of silica tetrahedra
type of cations
why arent all combos of geometry/ cation type stable
Fg/Mg cations are smaller than K/Ca/Na ones
what is present in silicates with every geometry of silica tetrahedra
Al
ex of a single tetrahedra silicate
olivine
ex of a single chain silicate
augite
ex of a double chain silicate
horneblende
examples of sheet silicates
biotite
muscovite
examples of 3d framework silicates
potassium feldspar
quartz
single tetrahedras, single chains, and double chain silicates form with… and are usually … in colour
Fe/Mg as cations
ferromagnesian
dark
sheet silicates form with…
EITHER Fe/Mg OR K/Ca/Na as cations
3D framework silicates form with… and are usually … in colour
K/Ca/Na anions
non ferromagnesian
light in colour
going from less (MAFIC) to more complex (FELSIC) silicate structures, … increases BUT … decreases
density increases
silica content decreases
forsterite
isolated tet. silicate
magnesium silicate
Mg2SiO4
fayalite
isolated tetrahedra
iron silicate
Fe2SiO4
olivine
isolated tet.
iron-magnesium silicate
FeMgSiO4
between forsterite and fayalite
single chain silicate mineral group example
pyroxene group → ex. augite
double chain silicate mineral group
amphibole → hornblende
mica sheet silicate group
covalent bonding within the sheet
ionic bonding between the sheets
perfect basal cleavage
muscovite- MICA sheet silicate group
non ferromagnesium silicate
sheets up to 3×5 m
used in metallic paint and makeup
biotite- MICA sheet silicate group
ferromagnesium silicate
perfect basal cleavage
black
used to date rocks
clay sheet silicate group
sheet silica minerals with water trapped between sheets
often formed by weathering of minerals like feldspar
kaolinite- CLAY sheet silica group
forms china clay
serpentine- CLAY sheet silicate group
formed via metamorphism of basalt
montmorillonite- CLAY sheet silicate group
forms bentonite
used in drilling mud
quartz group
3D framework silicate
continuously bonded SiO4
very abundant in Earths crust
feldspar group
interlinked tetrahedra of SiO4 and AlO4 anions (neg. charged framework)
metal cations in voids (K, Na, Ca)
2 orthogonal cleavages
light coloured
60% of crust
potassium feldspar
K-feldspar/ orthoclase
KAlSi3O8
no striations
plagioclase feldspar
if calcium- anorthite
if sodium- albite
occurs bc Ca and Na ions are similar in size
often has striations
carbonate group
anion is carbonate radical/ polyatomic ion
found mostly in the sedimentary rocks (limestone, dolostone)
derived from shells and hard parts of marine organisms
mostly associated w biomineralization (clams, snails, etc)
examples of carbonates
Calcite and Aragonite (CaCO3)
if tropical→ aragonite/ if temperate/cold → calcite
dolomite [CaMg(CO3)²]
sulphate group
sulphate radical in anion (SO4)
forms in desert from evaporation of water
can act as a weak layer where faulting localizes
ex. of sulphate group
gypsum (CaSO42H2O)
when dried/ compressed → anhydrite (CaSO4)
most rock forming minerals are…
ferromagnesian silicates
nonferromagnesian silicates
carbonates
sulfates
halides