Nacrite
{{short description|Phyllosilicate mineral: group of kaolinite}}
{{Infobox mineral
| name = Nacrite
| image = Nacrite - Mineralogisches Museum Bonn1.jpg
| alt =
| caption = Nacrite, "Frohe Hoffnung"-shaft, Wildental, Ore Mountains
| category = Phyllosilicates
Kaolinite-serpentine group
| formula = Al2Si2O5(OH)4
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| strunz = 9.ED.05
| system = Monoclinic
| class = Domatic (m)
(same H-M symbol)
| symmetry = Cc
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| references = [http://www.mindat.org/min-2826.html Mindat Data sheet][http://www.webmineral.com/data/Nacrite.shtml Webmineral data]
}}
Nacrite Al2Si2O5(OH)4 is a clay mineral that is polymorphous (or polytypic) with kaolinite.{{Cite web |title=Nacrite |url=https://soilsfacstaff.cals.wisc.edu/facstaff/barak/virtual_museum/nacrite/nacrite_tx.html |access-date=2024-12-18 |website=soilsfacstaff.cals.wisc.edu}} {{Cite web |title=Nacrite |url=https://www.mindat.org/min-2826.html |access-date=2024-12-18 |website=www.mindat.org}} It crystallizes in the monoclinic system. X-ray diffraction analysis is required for positive identification.
Nacrite was first described in 1807 for an occurrence in Saxony, Germany. The name is from nacre in reference to the dull luster of the surface of nacrite masses scattering light with slight iridescences resembling those of the mother of pearls secreted by oysters.
References
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{{Phyllosilicates}}
{{Clay minerals}}
Category:Polymorphism (materials science)
Category:Minerals in space group 9
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