Manganoeudialyte
| Manganoeudialyte | |
|---|---|
| General | |
| Category | Silicate mineral, Cyclosilicate |
| Formula (repeating unit) | Na14Ca6Mn3Zr3[Si26O72(OH)2]Cl2·4H2O |
| Crystal system | Trigonal, R3m |
| Unit cell | a=14.25, c=30.08 [Å] (approximated) |
| Identification | |
| Color | Pink to purple |
| Crystal habit | interstitial patches |
| Crystal symmetry | Trigonal - Ditrigonal Pyramidal (3m) |
| Cleavage | None |
| Fracture | Uneven |
| Tenacity | Brittle |
| Mohs scale hardness | 5-6 |
| Luster | Vitreous |
| Streak | White |
| Diaphaneity | Transparent or translucent |
| Density | 2.89-2.94 g/cm3 (measured) |
| Optical properties | Uniaxial (+) |
| Refractive index | nω=1.60 nε=1.61 (approximated) |
| Pleochroism | None |
| References | [1][2] |
Manganoeudialyte is an moderately rare mineral of the eudialyte group[1], with formula Na14Ca6Mn3Zr3Si2[Si24O72(OH)2]Cl2·4H2O. The formula given is one of the forms that can be given, based on the originally reported one, and shows dominance of silicon at both the M3 and M4 sites. As suggested by its name, it is the manganese-analogue of eudialyte.[2][3]
Occurrence and association
Manganoeudialyte was discovered in khibinites of the Poços de Caldas massif, Brazil.[2] Associated minerals are aegirine, analcime, astrophyllite, cancrinite, fluorite, lamprophyllite, nepheline, potassium feldspar, rinkite, sodalite, and titanite.[1]
Notes on chemistry
Impurities in manganoeudialyte include strontium, potassium, niobium, aluminium, fluorine, and minor hafnium, cerium,and lanthanum.[1][2]
References
- 1 2 3 4 Mindat, Manganoeudialyte, http://www.mindat.org/min-39640.html
- 1 2 3 4 Nomura, S.F., Atencio, D., Chukanov, N.V., Rastsvetaeva, R.K., Coutinho, J.M.V., and Karipidis, T.K., 2010: Manganoeudialyte - a new mineral from Poços de Caldas, Minas Gerais, Brasil. Zapisko RMO 4
- ↑ Handbook of Mineralogy, Manganoeudialyte, http://www.handbookofmineralogy.org/pdfs/manganoeudialyte.pdf
External links
This article is issued from Wikipedia - version of the Tuesday, April 26, 2016. The text is available under the Creative Commons Attribution/Share Alike but additional terms may apply for the media files.