| 词条 | Quenstedtite |
| 释义 |
| name = Quenstedtite | boxwidth = | boxbgcolor = | image = | imagesize = | alt = | caption = | category = sulfate minerals | formula = Fe2(SO4)3·11H2O | molweight = | strunz = 7.CB.65 | system = Triclinic | class = Pinacoidal ({{overline|1}}) (same H-M symbol) | symmetry = P{{overline|1}} | unit cell = a = 6.184 Å, b = 23.6 Å c = 6.539 Å; α = 94.18° β = 101.73°, γ = 96.27°; Z = 2 | color = white to very pale violet to red-violet | 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 = | prop1 = | prop1text = | references = [1] }}Quenstedtite is an uncommon iron sulfate mineral with chemical formula Fe2(SO4)3·11H2O. It forms violet or white triclinic crystals. Found in oxidized zones of pyrite-rich orebodies, especially in arid climates. It was first reported in 1888 for an occurrence in Tierra Amarilla, Copiapó Province, Atacama Region, Chile and named by G. Linck in 1889 for the German mineralogist F. A. von Quenstedt (1809–1889).[1][2] References1. ^1 Mindat 2. ^Handbook of Mineralogy
3 : Sulfate minerals|Iron minerals|Triclinic minerals |
| 随便看 |
|
开放百科全书收录14589846条英语、德语、日语等多语种百科知识，基本涵盖了大多数领域的百科知识，是一部内容自由、开放的电子版国际百科全书。