Fengchengite is a rare mineral of the eudialyte group with the formula . 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) and essential, site-dominating vacancies. The mineral was discovered in the Saima complex near Fengcheng city in China – hence its name.
{{infobox mineral | name = Fengchengite | category = Cyclosilicate | image = | imagesize = | alt = | caption = | formula = {{chem2|Na12[ ]3(Ca,Sr)6Fe3^{3+}Zr3Si(Si25O73)(H2O,OH)3(OH,Cl)2}} | IMAsymbol = Fcg | strunz = | dana = | system = Trigonal | class = Hexagonal scalenohedral (m) H-M symbol: ( 2m) | symmetry = Rm | 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 = }} Fengchengite is a rare mineral of the eudialyte group with the formula {{chem2|Na12[ ]3(Ca,Sr)6Fe3^{3+}Zr3Si(Si25O73)(H2O,OH)3(OH,Cl)2}}. 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) and essential, site-dominating vacancies. The mineral was discovered in the Saima complex near Fengcheng city in China – hence its name.
==References==
Discovered by embedding cosine similarity (sentence-transformers MiniLM, 384-dim).