Clinozoisite
From Wikipedia, the free encyclopedia
| Clinozoisite | |
|---|---|
Clinozoisite |
|
| General | |
| Category | Mineral |
| Chemical formula | {Ca2}{Al3}[O|OH|SiO4|Si2O7] |
| Crystal symmetry | 2/m - Prismatic |
| Identification | |
| Color | colorless, green, gray, light green, yellow green |
| Crystal system | monoclinic |
| Cleavage | perfect on {001} |
| Fracture | irregular/uneven |
| Mohs scale hardness | 7 |
| Luster | vitreous |
| Streak | grayish white |
| Diaphaneity | transparent, translucent |
| Specific gravity | 3.3 - 3.4 |
Clinozoisite is a mineral, a complex sorosilicate of calcium and aluminium and is usually a grey green colour.
Its formula is Ca2Al3[O|OH|SiO4|Si2O7].
It was originally discovered in 1896 in Tyrol, Austria, and is so-named because of its resemblance to zoisite.
Forms a continuous solid solution series with substitution of Fe(|||) for Al(|||). Only the m3 site accepts Fe(III) readily.
[edit] References
- Mineral Handbook
- Mindat
- Webmineral data
- Nesse, William D., "Introduction to Mineralogy," (c)2000 Oxford University Press ISBN 0-19-510691-1
| This article about a specific silicate mineral is a stub. You can help Wikipedia by expanding it. |