Frankamenite: Difference between revisions
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'''Frankamenite''' is the [[fluorine]]-dominate variation of the rare mineral [[canasite]] with a general formula of K<sub>3</sub>Na<sub>3</sub>Ca<sub>5</sub>(Si<sub>12</sub>O<sub>30</sub>)[F,(OH)]<sub>4</sub>·(H<sub>2</sub>O).<ref name=Mindat/> |
'''Frankamenite''' is the [[fluorine]]-dominate variation of the rare [[mineral]] [[canasite]] with a general formula of K<sub>3</sub>Na<sub>3</sub>Ca<sub>5</sub>(Si<sub>12</sub>O<sub>30</sub>)[F,(OH)]<sub>4</sub>·(H<sub>2</sub>O).<ref name=Mindat/> |
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Frankamenite belongs to the [[triclinic]] [[crystal system]], with the bases of its structure containing Ca-Na mixed octahedra joined by octagonal tubes SiO<sub>4</sub> of the composition (Si<sub>12</sub>O<sub>30</sub>). Frankamenite has six Ca-Na mixed positions distributed amongst these octahedra, reflecting its varying compositions.<ref>Rozhdestvenskaya, I.V. and Nikishova, L.V. (1996) The Crystal Structure of Frankamenite. Mineralogical Magazine; 60; 897-905.</ref> |
Frankamenite belongs to the [[triclinic]] [[crystal system]], with the bases of its structure containing Ca-Na mixed octahedra joined by octagonal tubes SiO<sub>4</sub> of the composition (Si<sub>12</sub>O<sub>30</sub>). Frankamenite has six Ca-Na mixed positions distributed amongst these octahedra, reflecting its varying compositions.<ref>Rozhdestvenskaya, I.V. and Nikishova, L.V. (1996) The Crystal Structure of Frankamenite. Mineralogical Magazine; 60; 897-905.</ref> |
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Revision as of 02:36, 1 May 2015
| Frankamenite | |
|---|---|
| General | |
| Category | Inosilicates |
| Formula (repeating unit) | K3Na3Ca5(Si12O30)[F,(OH)]4·(H2O) |
| Strunz classification | 09.DG.90 |
| Crystal system | Triclinic |
| Identification | |
| Color | Greenish blue, blueish gray, greenish gray, lilac grey |
| Crystal habit | Lath, columnar |
| Cleavage | Good on (010) and (100) |
| Tenacity | Brittle |
| Mohs scale hardness | 5.5 |
| Luster | Vitreous |
| Streak | Pale blue |
| Diaphaneity | Transparent to translucent |
| Specific gravity | 2.68 |
| Optical properties | Biaxial positive |
| Refractive index | nα = 1.536 nβ = 1.539 nγ = 1.542 |
| Birefringence | 0.0060 |
| Dispersion | r < v strong |
| References | [1][2] |
Frankamenite is the fluorine-dominate variation of the rare mineral canasite with a general formula of K3Na3Ca5(Si12O30)[F,(OH)]4·(H2O).[1]
Frankamenite belongs to the triclinic crystal system, with the bases of its structure containing Ca-Na mixed octahedra joined by octagonal tubes SiO4 of the composition (Si12O30). Frankamenite has six Ca-Na mixed positions distributed amongst these octahedra, reflecting its varying compositions.[3]
Frankamenite was named for the Russian mineralogist-crystallographer V. A. Frank-Kamentsky (1915–1994), who discovered the mineral.[2]
Frankamenite occurs in association with the rare mineral charoite, which is found only in the Sakha Republic, Yakutia, Siberia, Russia. Here, metasomatism enriches a syenite massif with potassium when it comes into contact with a limestone at around 200–250 °C. This metamorphic process produces a potassium feldspar metasomatite, the typical geological environment for canasite and, therefore, frankamenite. Frankamenite and charoitein are exclusive to the Sakha Republic in this sort of environment, as mineralogists have yet to discover the minerals elsewhere.[4]
References
- ^ a b Mindat.org
- ^ a b Webmineral data
- ^ Rozhdestvenskaya, I.V. and Nikishova, L.V. (1996) The Crystal Structure of Frankamenite. Mineralogical Magazine; 60; 897-905.
- ^ Charoite on Webmineral
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