| 词条 | Fengchengite |
| 释义 |
| name = Fengchengite | category = Cyclosilicate | image = | imagesize = | alt = | caption = | formula = Na12[]3(Ca,Sr)6Fe33+Zr3Si(Si25O73)(H2O,OH)3(OH,Cl)2 | strunz = | dana = | system = Trigonal | class = Hexagonal scalenohedral ({{overline|3}}m) H-M symbol: ({{overline|3}} 2m) | symmetry = R{{overline|3}}m | unit cell = a = 14.25, c = 30.03 [Å] (approximated) | color = | colour = | habit = | twinning = | cleavage = | fracture = | tenacity = | mohs = | luster = | streak = | diaphaneity = | gravity = | density = | polish = | opticalprop = | refractive = | birefringence = | pleochroism = | 2V = | dispersion = | extinction = | length fast/slow = | fluorescence = | absorption = | melt = | fusibility = | diagnostic = | solubility = | impurities = | alteration = | other = | references = [1][2] }} Fengchengite is a rare mineral of the eudialyte group[1] with the formula Na12[]3(Ca,Sr)6Fe33+Zr3Si(Si25O73)(H2O,OH)3(OH,Cl)2.[2][1] The formula is simplified as it does not show the presence of cyclic silicate groups. When compared to other minerals of the group, fengchengite characterizes in the presence of ferric iron (thus similar to ikranite, mogovidite and feklichevite[1]) and essential, site-dominating vacancies. The mineral was discovered in the Saima complex near Fengcheng city in China - hence its name.[1][2] References1. ^1 2 3 4 Mindat, Fengchengite, http://www.mindat.org/min-42378.html 2. ^1 2 Shen, G., Xu, J., Yao, P., and Li, G., 2011. Fengchengite, IMA 2007-018a. CNMNC Newsletter No. 11, December 2011, 2892; Mineralogical Magazine 75,2887-2893 Further reading
6 : Calcium minerals|Cyclosilicates|Iron minerals|Sodium minerals|Zirconium minerals|Trigonal minerals |
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