Humite: Difference between revisions
m robot Adding: zh:矽鎂石 |
add information about the humite group |
||
Line 3: | Line 3: | ||
It was first described in 1813 and named for [[Abraham Hume]] (1749-1838). |
It was first described in 1813 and named for [[Abraham Hume]] (1749-1838). |
||
Humite is also used as the name of a group of closely related minerals -- humite, [[clinohumite]], [[chondrodite]], and [[norbergite]]. These minerals are similar in structure and in chemistry. Deer et al. (1997) note that a general formula for the humite-group minerals can be simply expressed as nM<sub>2</sub>SiO<sub>4</sub> . M(OH,F)<sub>2</sub> , where M is Mg, Fe, Ti etc. and n = 1 (norbergite), 2 (chondrodite), 3 (humite), and 4 (clinohumite). Deer et al. (1997) also note that although the formula above correctly describes the chemistries of these minerals, structural formulas are more complex. |
|||
==See also== |
==See also== |
||
* [[Jerrygibbsite]] |
* [[Jerrygibbsite]] |
||
==References== |
|||
*Deer, W. A., Howie, R. A., and Zussman, J., 1997, ''Rock-forming minerals: Volume 1A, Second Edition, Orthosilicates.'' The Geological Society, Bath, UK. ISBN 1-897799-8-8 |
|||
==External links== |
==External links== |
Revision as of 19:35, 28 June 2008
Humite is an orthorhombic mineral of a transparent vitreous brown to orange color. It is found in the volcanically ejected masses of Vesuvius. It is a nesosilicate of iron and magnesium which also contains fluorine and hydroxide. The formula is: (Mg,Fe)7(SiO4)3(F,OH)2.
It was first described in 1813 and named for Abraham Hume (1749-1838).
Humite is also used as the name of a group of closely related minerals -- humite, clinohumite, chondrodite, and norbergite. These minerals are similar in structure and in chemistry. Deer et al. (1997) note that a general formula for the humite-group minerals can be simply expressed as nM2SiO4 . M(OH,F)2 , where M is Mg, Fe, Ti etc. and n = 1 (norbergite), 2 (chondrodite), 3 (humite), and 4 (clinohumite). Deer et al. (1997) also note that although the formula above correctly describes the chemistries of these minerals, structural formulas are more complex.
See also
References
- Deer, W. A., Howie, R. A., and Zussman, J., 1997, Rock-forming minerals: Volume 1A, Second Edition, Orthosilicates. The Geological Society, Bath, UK. ISBN 1-897799-8-8