bystrite
{{short description|Feldspathoid mineral in the cancrinite subgroup}}
{{Infobox mineral
| name = Bystrite
| category = Tectosilicate minerals, feldspathoid group, cancrinite group
| image =
| alt =
| caption =
| formula = (Na,K)7Ca(Si6Al6)O24S4.5•(H2O)
| molweight =
| strunz = 9.FB.05
| dana = 76.02.05.02
| system = Trigonal
| class = Ditrigonal pyramidal (3m)
H-M symbol: (3m)
| symmetry = P31c
| color = Yellow
| colour =
| habit = Tabular to irregular grains and inclusions
| twinning =
| cleavage = {10{{overline|1}}0} Good
| fracture =
| tenacity =
| mohs = 5
| luster = Vitreous
| streak = light yellow
| diaphaneity = Transparent to translucent
| gravity = 2.43
| density =
| polish =
| opticalprop = Uniaxial (+)
| refractive = nω = 1.584 nε = 1.660
| birefringence = δ = 0.076
| pleochroism = Deep yellow to colorless
| 2V =
| dispersion =
| extinction =
| length fast/slow =
| fluorescence=
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| melt =
| fusibility =
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| solubility =
| other =
| alteration =
| references = [https://www.mineralienatlas.de/lexikon/index.php/MineralData?mineral=Bystrite Mineralienatlas]http://rruff.geo.arizona.edu/doclib/hom/bystrite.pdf Handbook of Mineralogyhttp://webmineral.com/data/Bystrite.shtml Webmineral datahttp://www.mindat.org/min-813.html Mindat.org
}}
Bystrite is a silicate mineral with the formula (Na,K)7Ca(Si6Al6)O24S4.5•(H2O), and a member of the cancrinite mineral group. It is a hexagonal crystal, with a 3m point group. The mineral may have been named after the Malaya Bystraya deposits in Russia, where it was found.
Bystrite is a cancrinite mineral and exhibits similar physical properties, composition and structure as other cancrinites.
Structure
Bystrite has a structure that is shared with many of the minerals in the cancrinite group. It exhibits a hexagonal crystal structure with a 3m point group. Bystrite also has a P31c space group. The structure of bystrite could not be easily found due to the mineral exhibiting a strong pseudotranslation, therefore, mineralogists made a model to find out the internal structure of the bystrite mineral, the idea was based on analyzing the tetrahedral frameworks of cancrinite minerals, and it did yield accurate results in predicting the structure of the mineral. Bolotina et al. (2004){{Citation needed|date=January 2010}}
Geologic occurrence
The most studied sample of the mineral was found in the Malaya Bystraya deposit in Russia. Bystrite occurs in lazurite deposits, and is usually associated with lazurite, calcite, and diopside.Kretz, Ralph. (2001) Bystrite (Na, K)7Ca(Si6Al6)O24S1.5.H2O. Mineral Data Publishing, 1.2.
The mineral is not very widely spread, either that or it has not been really searched for due to the lack of importance or significance. There is only one bystrite deposit that was mentioned in the literature, and that deposit is found in the Malaya Bystraya lazurite deposit located {{convert|25|km|abbr=on}} to the west of Slyudyanka, and just south of Lake Baikal in Russia.
Literature survey
The first paper addressing Bystrite was by Sapozhnikov, et al. and was originally written in Russian, but mineral data publishing translated most of the important information to English in 2001.Sapozhnikov, A.N., V.G. Ivanov, L.F. Piskunova, A.A. Kashaev, L.E. Terentieva, and E.A. Pobedimskaya. (1991) Bystrite Ca(Na, K)7(Si6Al6O24)(S3)1.5.H2O - A new cancrinite-like mineral. Zap. Vses. Mineral. Obshch., 120(3), 97-100. Referenced in Kretz, Ralph. (2001) Bystrite (Na, K)7Ca(Si6Al6)O24S1.5.H2O. Mineral Data Publishing, 1.2.