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Mineral Science

TermDefinition
parallel growth series of crystals with their crystallographic axes and faces parallel
epitaxial growth when two different crystalline substances show a non-random overgrowth
twinning symmetrical intergrowth of two or more crystals of the same substance
contact twin individuals in contact with each other along a twin plane
penetration twin irregular compositional surface & twin law usually defined by a twin axis direction
isostructuralism same structure, different chemistry. ex: halite and galena
polymorphism same chemistry, different structures (dealing with temperature/ pressure changes)
reconstructive polymorphism diamond & graphite. both made of carbon, but different amounts of pressure were added when they formed
displacive polymorphism temperature changes
order-disorder polymorphism very common in metals (k-feldspar (cd))
polytypism special type of polymorphism occurs when 2 polymorphs differ only in the stacking of identical, 2-dimensional sheets or layers (cd)
metamict minerals form as a crystalline solid but their crystal structure has been destroyed by radiation. ex: uraninite breaks down to glass "pitchblende"
mineraloid (noncrystalline minerals) no long-range order in structure. ex: opal
pseudomorphism "false form" existence of a mineral with the outward crystal form of another mineral species
substitutional pseudomorphism gradual removal of original material and simultaneous replacement of it by another with no chemical reaction between the 2
encrustation pseudomorphism one mineral deposited over another. ex: quartz over fluorite
alteration pseudomorphism chemical change. use some of the chemistry, introduce something new and kick something else out
growth twins result of the emplacement of atoms, or ions on the outside of a growing crystal in an interrupted arrangement (accidents of growth)
transformation twins occurs in preexisting crystals and represent secondary twinning (heat)
deformation pressure causes layers in structure to glide to new positions. ex: calcite twinning
matter anythings that has mass and occupies space. gas, liquid, solid
atom smallest subdivision of matter that retains the characteristics of the element
anion gains electrons and is negative in charge
cation lose electrons and is positive in charge
ionization potential the amount of energy necessary to remove electrons
electronegativity measure of the ability of an atom in a crystal structure of molecule to attract electrons to its outer shell
interstitial solid solution ions fitting intro structural voids. ex: water softener
omission solid solution higher charged cation substituting for lower charged one (open/ vacant site)
coupled solid solution charge must be the same on both side of the equation
phase a homogeneous substance with a well defined set of physical and chemical properties
phase diagram represents stability ranges of phases (gas, liquid, solid) under variable external conditions
component minimum number of chemical species needed to define the range of phase compositions in the system
triple point where the 3 lines meet; no degrees of variation
acicular slender, needle-like crystals
capillary hair like or threadlike crystals
bladed elongated crystals flattened like a knife blade
dendritic arborescent, in slender divergent branches
reticulated lattice like groups of slender crystals
divergent/ radiated radiating crystal group
drusy surface covered with a layer of small crystals
columnar stout, column like individuals
fibrous an aggregate of many flattened blades
stellated radiating individuals forming star-like or circular groups
globular radiating individuals forming small spherical or hemispherical groups
botryoidal globular forms resembling "bunches of grapes"
reniform radiating individuals terminating in round kidney-shaped masses
mammillary large rounded masses resembling mammae, formed by radiating individuals
colloform spherical forms composed of radiating individuals without regard to size
foliated easily separable into plates or leaves
micaceous similar to foliated but splits into exceedingly thin sheets
lamellar/ tabular flat, plate like individuals superimposed upon each other
plumose feather-like structure
granular mineral aggregate composed of equant grains
concentric spherical layers superimposed upon one another about a common center
pisolitic rounded masses about the size of peas
oolitic aggregate formed of small spheres
cleavage tendency of a mineral to break parallel to atomic planes
parting breakage along planes of structural weakness. result from pressure, twinning or exsolution
fracture some crystal structures have equal bond strength on all directions, therefore crystalline mineral breaks: conchoidal fracture, fibrous (splintery), hackley (jaagged), or uneven
relative density ratio of the weight of a substance and the weight of an equal volume of water at 4 degrees C
Z number of formula units/ unit cell
M molecular weight of substance
N avogadros number
V volume of unit cell
Density = (ZxM)/(NxV)
Created by: 1357915501
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