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About: Clinozoisite     Goto   Sponge   NotDistinct   Permalink

An Entity of Type : yago:WikicatAluminiumMinerals, within Data Space : dbpedia.org associated with source document(s)

Type: Thingdul:ChemicalObjectchemical substanceMineralmineralyago:WikicatCalciumMineralsyago:WikicatMineralsyago:WikicatMonoclinicMineralsyago:WikicatSilicateMineralsyago:WikicatSilicatesyago:Abstraction100002137yago:Chemical114806838yago:Compound114818238yago:Material114580897yago:Matter100020827yago:Mineral114662574yago:Part113809207yago:PhysicalEntity100001930yago:Relation100031921yago:WikicatHydroxideMineralsyago:Salt115010703yago:Silicate115040033yago:Substance100019613yago:WikicatAluminiumMinerals New Facet based on Instances of this Class

Clinozoisite is a complex calcium aluminium sorosilicate mineral with formula: Ca2Al3(Si2O7)(SiO4)O(OH). It forms a continuous solid solution series with epidote by substitution of iron(III) in the aluminium (m3 site) and is also called aluminium epidote. Clinothulite is a manganese bearing variety with a pinkish hue due to substitution of Mn(III) in the aluminium site. It was originally discovered in 1896 in East Tyrol, Austria, and is so-named because of its resemblance to zoisite and its monoclinic crystal structure.