Mineralogy Flashcards
Mohs Scale, 1-10
Talc, gypsum, calcite, flourite, apatite, orthoclase, quartz, topaz, corrundum, diamond
Diaphaneity
Mineral transmits light
Asterism
Inclusions of tiny parallel slender fibers, refraction
Pleochroism
Different colors at different angles
Chatoyancy
Light reflection from luminous band
The law of the constancy of interfacial angles
The angles between the crystal faces of a given species are constant, whatever the lateral extension of these faces and the origin of the crystal, and are characteristic of that species.
Unit cell
The smallest subset of the lattice that still retains all of the physical, chemical, and symmetry properites of the mineral.
Isometric
The crystallographic axes used in this system are of equal length and are mutually perpendicular, occurring at right angles to one another.
Tetragonal
The tetragonal system also has three axes that all meet at 90º. C shortest
Orthorhomic
All three bases intersect at 90° angles, a=b X c
Hexagonal
The C or vertical axis is at 90º to the shorter axes, a X b X c. 90/90/120
Triclinic
In the triclinic system, all the axes are different lengths. None of them meet at 90º B/a/y
Quartz
SiO2 Hexagonal 1
Orthoclase
KAlSi3O8 Monoclinic 2
Albite
NaAlSi3O8 Monoclinic/Triclinic 3
Anorthite
CaAlSi3O8 Triclinic 4
Muscovite
KAl2(AlSi3O10)(OH)2 Monoclinic 5
Biotite
K(Mg,Fe)3(AlSi3O10)(OH)2 Monoclinic 6
Amphibole
(Ca,Mg,Fe)7Si8O22)(OH)2 Monoclinic 7
Pyroxene
(Ca,Mg,Fe)2Si2O4 Orthorhombic/Monoclinic 8
Olivines
(Mg,Fe)2SiO4 Orthorhombic 9
Calcite
CaCO3 Hexagonal 10
Crust
Oxygen, Silicon, Aluminum
Upper Mantle
Silicon, oxygen, magnesium, and iron. Olivines and pyroxenes
Lower Mantle
Iron, magnesium, and silicates
Outer Core
Iron and nickel
Inner Core
Fe, Ni
Radius Ratio, why care?
Radius ratio is the ratio of radius of the cation to the radius of the anion. We care because larger anions can have more cations, then determines the coordination.
Orthopyroxene
Fe, Mg
Clinopyroxene
Ca,
Silicates are classified by
arrangement of silicate tetrahedra, Neo, Soro, Cyclo, Chain single and double, hydro, Phyllo, and Tecto
Neosilicates
1:4 Si:O each tetrahedron is isolated