Feldspars, feldspathoids, zeolites
Feldspar phase relations, exsolution, etc.
Finish materials left over from previous lecture.
- Feldspar structure movies
- Phase equilibria
- What happens in lower silica environments? (Figs. 13.137, 9.8b, 9.10, 9.14)
Feldspathoids
- anhydrous framework silicates
- composition reflects formation from low silica, high alkali melts
- structures related to feldspars but with 6-membered rings leading to more
open structures and lower densities
- some feldspathoids contain unusual anions such as Cl-,
S=, SO4-2,
and CO3-2
Leucite: tetragonal below 600°C; cubic above
Nepheline: hexagonal; related to high tridymite structure
Sodalite: cubic
- Sodalite (217K) Na3Al3Si3O12 (NaCl) (Na-yellow, Al-aqua, Si-blue, O-red, Cl-green)
Scapolite Series
- metamorphic minerals
- complete solid solution between Marialite (3NaAlSi3O8.NaCl) and Meionite (3CaAl2Si2O8.CaCO3 or CaSO4)
- this is a good way to remember the formula but not the structures
- Na for Ca solid solution compensated for by Si for Al solid solution
- minerals are tetragonal
- imperfect but distinct cleavage, more fibrous in appearance than feldspar cleavage
Zeolites
- hydrous framework aluminosilicates
- large voids in structure containing Na+, Ca+2,
K+, and H2O
- filling cavities and veins in basic igneous rocks
- alterations of volcanic tuffs and glasses
- low grade metamorphic rocks - "zeolite facies"
- soft, low density
- some fibrous (chains); some platy (sheets); some equant (frameworks)
- used as molecular seives and cation exchange resins
Analcime: cubic; very similar to feldspathoids
Natrolite: orthorhombic; prismatic to acicular, radiating crystals common
- Natrolite (499K) Na2Al2Si3O10.2H2O (Na-yellow, Al-aqua, Si-blue, O-red, H2O-brown)
Chabazite: hexagonal; used as a molecular seive
These were created on the CrystalMaker 1.1.4 interactive crystallography program
. If you would like more information on the program, please contact:
David Palmer
(Technical information)