Movatterモバイル変換


[0]ホーム

URL:


Log InRegister
AboutSupport UsPhotosDiscussionsSearchLearnMore
Quick Links :The Mindat ManualThe Rock H. Currier Digital LibraryMindat Newsletter [Free Download]
Home PageAbout MindatThe Mindat ManualHistory of MindatCopyright StatusWho We AreContact UsAdvertise on Mindat
Donate to MindatCorporate SponsorshipSponsor a PageSponsored PagesMindat AdvertisersAdvertise on Mindat
Learning CenterWhat is a mineral?The most common minerals on earthInformation for EducatorsMindat ArticlesThe ElementsThe Rock H. Currier Digital LibraryGeologic Time
Minerals by PropertiesMinerals by ChemistryAdvanced Locality SearchRandom MineralRandom LocalitySearch by minIDLocalities Near MeSearch ArticlesSearch GlossaryMore Search Options
Search For:
Mineral Name:
Locality Name:
Keyword(s):
 
The Mindat ManualAdd a New PhotoRate PhotosLocality Edit ReportCoordinate Completion ReportAdd Glossary Item
Mining CompaniesStatisticsUsersMineral MuseumsClubs & OrganizationsMineral Shows & EventsThe Mindat DirectoryDevice SettingsThe Mineral Quiz
Photo SearchPhoto GalleriesSearch by ColorNew Photos TodayNew Photos YesterdayMembers' Photo GalleriesPast Photo of the Day GalleryPhotography

Muscovite

A valid IMA mineral species - grandfathered
This page kindly sponsored in memory of Laszlo Z. Valachi
Photos of Muscovite (2429)Discuss Muscovite
Muscovite GallerySearch Photos of Muscovite
EditAdd SynonymEdit CIF structuresClear Cache
KAl2(AlSi3O10)(OH)2
Colour:
White to colorless, silvery-white, and tinged various colors by impurities.
Lustre:
Vitreous, Silky, Pearly
Hardness:
Specific Gravity:
2.77 - 2.88
Crystal System:
Monoclinic
Member of:
Name:
The earliest names attributable to muscovite include Muscovy Glass, Cat Silver, and Lapis Specularis (stone mirror); these names appearing in texts in the seventeenth century and before. The stand-alone name 'Muscovite' was used as early as 1794 by Johann Gottfried Schmeisser in his System of Mineralogy and is derived from the term "Muscovy glass," which was in common use by that time. Muscovy Province in Russia yielded sheet mica for a variety of uses. Muscovite and sometimes similar species were earlier called mica (Phillips and Kersey, 1706), glimmer (Phillips and Kersey, 1706), and isinglass (1747 according to OED) but all of these terms are still in use to some degree. It should be noted that mica, glimmer, and isinglass were also used for a variety of materials before these given dates and in those earlier times did not always indicate what would be a mineral, much less muscovite proper. Isinglass, for example, was originally used for a gelatinous bladder found in sturgeon.
Mica Group.

The most common of the Mica Group minerals, it is typically found as massively crystalline material in "books" or in flaky grains as a constituent of many rock types. It is clear with a pearly luster on cleavage faces, often having a sparkly look in rocks.
Several polytypes are known (see below); the most common one is the 2M1 polytype.

It can form a continuous series withceladonite andaluminoceladonite; intermediates are known as the varietyphengite and K-deficient variants asillite.

May be confused withmargarite and several lithium micas.




Unique Identifiers
IMA Formula:
KAl2(Si3Al)O10(OH)2

Classification of Muscovite

9 : SILICATES (Germanates)
E : Phyllosilicates
C : Phyllosilicates with mica sheets, composed of tetrahedral and octahedral nets
Dana 7th ed.:
71.2.2.1
71.2.2a.1

71 : PHYLLOSILICATES Sheets of Six-Membered Rings
2 : Sheets of 6-membered rings with 2:1 layers
16.3.8

16 : Silicates Containing Aluminum and other Metals
3 : Aluminosilicates of K

Mineral SymbolsJolyon RalphUnited Kingdom

Physical Properties of Muscovite
Transparency:
Transparent, Translucent
Colour:
White to colorless, silvery-white, and tinged various colors by impurities.
Streak:
White
Hardness Data:
Measured
Comment:
2.5 parallel to [001], 4 perpendicular to [001]
Tenacity:
Elastic
Cleavage:
Perfect
Perfect on {001}.
Parting:
On {110} and {010}.
Fracture:
Micaceous
Density:
2.77 - 2.88 g/cm3 (Measured)    2.83 g/cm3 (Calculated)

Optical Data of Muscovite
Surface Relief:
Moderate
Dispersion:
r > v weak
Optical Extinction:
Z = b; X ∧ c = 0°-5°; Y ∧ a = 1°-3°.
Pleochroism:
Weak
Comments:
Weak when colored
Comments:
Absorption: Faint, Y ≃ Z > X.

Chemistry of Muscovite
Common Impurities:
Cr,Li,Fe,V,Mn,Na,Cs,Rb,Ca,Mg,H2O

Age distribution
Click on an icon to view
Muscovite no.7 - Goldschmidt (1913-1926)
Muscovite no.12 - Goldschmidt (1913-1926)
3d models and HTML5 code kindly provided bywww.smorf.nl.

Toggle
Edge Lines |Miller Indices |Axes

Transparency
Opaque |Translucent |Transparent

View
Along a-axis |Along b-axis |Along c-axis |Start rotation |Stop rotation

Crystal Structureunknown 274
Data courtesy of RRUFF project at University of Arizona, used with permission.
Powder Diffraction Data:
d-spacingIntensity
10.01 Å(100)
5.02 Å(60)
4.48 Å(60)
4.46 Å(70)
3.35 Å(100)
3.21 Å(50)
2.59 Å(50)
2.56 Å(90)
Comments:
Data given are for the -2M^1 polytype.

Geological Environment

Other Language Names for Muscovite

Varieties of MuscoviteAl-illite-hydromicaVariety of Illite very low in K and high in water.AlurgiteName introduced by Breithaupt in 1865 and characterized by Penfield in 1893 (vide Knurr and Bailey, 1986). Placed by W. T. Schaller (1950) as an intermediate between leucophyllite (now a synonym of aluminoceladonite) and muscovite. A study of Knurr and Ba...AmmersooiteA variety of Illite capable of fixing Potassium, from Dutch fields.AstroliteSpherical aggregates composed of radiating tabular crystals.

Originally described from Pelz quarry, Diabase quarries, Neumark, Reichenbach, Vogtland, Saxony, Germany.AvaliteA chromian variety of Illite.
Originally described from Mt Avala, Belgrade, Serbia.Barium- and Chromium-bearing MuscoviteA barium- and chromium-bearing muscovite.Barium-Vanadium-MuscoviteA barian vanadian variety of Muscovite.

Originally reported from Silver Knob, Fish Camp, Yosemite Valley, Mariposa Co., California, USA.Barium-bearing MuscoviteA barium-rich variety ofmuscovite; probably equivalent tooellacherite; part of the series between muscovite andganterite.BatcheloriteA green slaty mineral, originally described by W.F. Petterd (1910) from the Mt. Lyell mine, Tasmania. Re-analysis of visually identical material from the same locality by Bothwell and Moss (1957) showed it to be a slightly Cr-bearingmuscovite, giving the...ChacaltaîteA green chlorite-like varety of muscovite.

Originally reported from Chacaltaya mine, Mt. Huayna Potosí (Huaina Potosi), Murillo Province, La Paz Department, Bolivia.Chromium-bearing SericiteA chromium-bearing variety of sericite. See alsofuchsite.Cr–Ni-rich illiteAlkali-deficient, dioctahedral mica with <14% NiO and <11wt.% Cr2O3DamouriteVery fine-grained, compact muscovite - with a greasy feel, "serpentine-like," and often a fibrous appearance when viewed from a certain direction.Degraded illiteIllite that has lost much of its potassium as the result of prolonged leaching.

Ref: AGIFerrimuscoviteA variety of muscovite rich in ferric iron.FuchsiteGreenish, Cr-bearing variety of muscovite (trivalent Cr replaces Al in the crystal structure). Note that trivalent V can also cause a greenish colour in muscovite (cf.vanadian muscovite,roscoelite).
Comparemariposite, a Cr-bearing phengite.

Originally...GieseckitePseudomorphs of muscovite after an unknown mineral.

Compare alsoliebenerite.GilbertiteCompact variety ofmuscovite.
The original chemical analysis of material from Stenagwyn, Cornwall, indicated no potassium or sodium ( Thomson, 1831). There were major amounts of silica and alumina, and minor amounts of CaO, MgO, and FeO. Thomson seems to...IlliteIllite is a very commonmica andclay mineral, typically found as extremely fine-grained masses of grayish-white to silvery-gray, sometimes greenish-gray, material. The literature on "illite" is very large as it is a widespread component of many sediments...Illite JadeA dense variety of illite with reddish banding (caused by microscopic inclusions ofhematite), which is used for carving and as an ornamental stone. In addition to hematite, the material usually also contains small quantities of impurities such asquartz,...Iron(II)-bearing muscoviteAn Fe(II)-bearing variety of muscovite.LeverrieriteAkaolinite-groupclay.
Originally reported from Saint-Etienne, Loire, Rhône-Alpes, France.

LiebeneriteMuscovite pseudomorphous afternepheline, possibly also aftercordierite.

Compare alsogieseckite.Lithian MuscoviteA lithium-bearing variety ofMuscovite.
A red muscovite does not necessarily imply that the muscovite is lithium rich. Chemical analyses have indicated that muscovite can be pink, not due to Li content, but rather the color is due to the dominance of Mn3+...Lithium Muscovite (of Levinson)Supposedly a lithian muscovite with 3-4% Li2O.

Note that this composition is probably a Li-poortrilithionite.MaripositeA greenish Cr-bearing "phengite". See alsofuchsite.

Originally described from Mariposa Co., California, USA.OellacheriteA green to colorless, Ba-bearing/rich variety ofmuscovite; it forms a complete series withganterite.PersbergiteMuscovite pseudomorphous afternepheline.

Not to be confused withpajsbergite.PhengitePhengite is an aluminous true mica which contains a relatively high amount of tetrahedrally co-ordinated Si (>3.1 apfu). As the Si amount increases, additional octahedrally co-ordinated cations are necessary for charge balance. This is an uncommon conditi...Rubidium-bearing MuscoviteRubidium-bearing muscovite with Rb2O contents of 1 and more mass%. Usual rock-forming mineral in late stages of the evolution of many granitic rare-metal (Ta,Be,Cs) natro-lithian pegmatites.SchernikiteA pink variety of muscovite, described by Bowman (1902).SericiteA term for a fine-grained white, pale green to oily greenish mica, mainlyMuscovite (rarelyParagonite).Star muscoviteMuscovite forming star-shaped crystal aggregates.
Especially nice specimens come from pegmatites in the Jenipapo district, Minas Gerais, Brazil.Vanadium-bearing IlliteA V-enriched "illite".Vanadium-bearing MuscoviteA V3+-bearing variety ofmuscovite.
Al-dominant member of the muscovite-roscoelite solid-solution range.VerditeTrade name for a green ornamental stone, primarily an impurefuchsite mica originally from North Kaap river, Kaap Station, South Africa.

Consists primarily of Fuchsite with minorAlbite,Chlorite Group,Corundum,Diaspore,Margarite,Quartz,Rutile andT...WilsoniteDescribed as an Mn-bearing "sericite" or muscovite pseudomorph afterscapolite. Hey lists it as an aluminosilicate of Mg and K.
Zinc-bearing MuscoviteZn-bearing variety from the "Mixed Series" formation, Nežilovo, Macedonia. Associates, i.a., withferricoronadite.

Relationship of Muscovite to other Species
Other Members of Dioctahedral mica:
BoromuscoviteKAl2(BSi3O10)(OH)2Mon. 2/m
Celadonite SubgroupA subgroup of the dioctahedralmica group.
ChromphylliteKCr2(AlSi3O10)(OH)2Mon. 2/m :B2/b
GlauconiteK0.60-0.85(Fe3+,Mg,Al)2(Si,Al)4O10](OH)2
NanpingiteCsAl2(AlSi3O10)(OH,F)2Mon. 2/m :B2/b
Natro-glauconite(Na,K)(Fe3+,Al,Mg)2((Si,Al)4O10)(OH)2
ParagoniteNaAl2(AlSi3O10)(OH)2Mon.
RoscoeliteKV3+2(AlSi3O10)(OH)2Mon. 2/m :B2/b
Tobelite(NH4)Al2(AlSi3O10)(OH)2Mon. 2/m :B2/m
Forms a series with:

Common AssociatesTric.1 :P19.EC.BalestraiteKLi2V5+Si4O12Mon. 2 :B29.EC.05TalcMg3Si4O10(OH)2Tric.1 :P19.EC.05MinnesotaiteFe2+3Si4O10(OH)2Tric.1 :P19.EC.05WillemseiteNi3Si4O10(OH)2Mon.9.EC.9.EC.VoloshiniteRb(LiAl1.50.5)(Al0.5Si3.5)O10F2Mon. 2/m :B2/b9.EC.10FluorluanshiweiiteKLiAl1.5(Si3.5Al0.5)O10F2Mon. 2/m :B2/m9.EC.10GarmiteCsLiMg2(Si4O10)F2Mon.9.EC.10GorbunoviteCsLi2(Ti,Fe)Si4O10(F,OH,O)2Mon.9.EC.10FerripyrophylliteFe3+Si2O5(OH)Mon. 2/m9.EC.10ManganiceladoniteK(MgMn3+◻)(Si4O10)(OH)2Mon.9.EC.10LuanshiweiiteKLiAl1.5(Si3.5Al0.5)O10(OH)2Mon. 2/m :B2/b9.EC.10PyrophylliteAl2Si4O10(OH)2Tric.19.EC.15ParagoniteNaAl2(AlSi3O10)(OH)2Mon.9.EC.15FerroaluminoceladoniteK(Fe2+Al◻)(Si4O10)(OH)2Mon. 2/m :B2/m9.EC.15NanpingiteCsAl2(AlSi3O10)(OH,F)2Mon. 2/m :B2/b9.EC.15FerroceladoniteK(Fe2+Fe3+◻)(Si4O10)(OH)2Mon. 2/m :B2/m9.EC.15Ganterite(Ba,Na,K)(Al,Mg)2(AlSi3O10)(OH)2Mon. 2/m :B2/b9.EC.15KreiteriteCsLi2Fe3+(Si4O10)F2Mon.9.EC.15RoscoeliteKV3+2(AlSi3O10)(OH)2Mon. 2/m :B2/b9.EC.15AluminoceladoniteK(MgAl◻)(Si4O10)(OH)2Mon. 2/m :B2/m9.EC.15Tobelite(NH4)Al2(AlSi3O10)(OH)2Mon. 2/m :B2/m9.EC.15TainioliteKLiMg2(Si4O10)F2Mon. 2/m :B2/m9.EC.15CeladoniteK(MgFe3+◻)(Si4O10)(OH)2Mon. 2/m :B2/m9.EC.15ChromceladoniteK(MgCr◻)(Si4O10)(OH)2Mon. 2 :B29.EC.15Montdorite(K,Na)2(Fe2+,Mn2+,Mg)5(Si4O10)2(OH,F)4Mon. 2/m :B2/m9.EC.15ChromphylliteKCr2(AlSi3O10)(OH)2Mon. 2/m :B2/b9.EC.15BoromuscoviteKAl2(BSi3O10)(OH)2Mon. 2/m9.EC.15UM1988-22-SiO:AlCaFFeHKLiMgKLiMgAl2Si3O10F2Mon.9.EC.15Chernykhite(Ba,Na)(V3+,Al,Mg)2((Si,Al)4O10)(OH)2Mon.9.EC.20MasutomiliteK(LiAlMn2+)[AlSi3O10]F2Mon. 2 :B29.EC.20OxyphlogopiteK(Mg,Ti,Fe)3[(Si,Al)4O10](O,F)2Mon. 2/m :B2/m9.EC.20Chloroferrokinoshitalite(Ba,K)(Fe2+,Mg)3(Al2Si2O10)(Cl,OH,F)29.EC.20SiderophylliteKFe2+2Al(Al2Si2O10)(OH)2Mon.9.EC.20SokolovaiteCsLi2Al(Si4O10)F2Mon.9.EC.20HendricksiteKZn3(Si3Al)O10(OH)2Mon. 2/m :B2/m9.EC.20TetraferriphlogopiteKMg3(Fe3+Si3O10)(OH,F)2Mon. 2/m :B2/m9.EC.20FluoranniteKFe2+3(Si3Al)O10F2Mon. 2/m :B2/m9.EC.20AspidoliteNaMg3(AlSi3O10)(OH)2Mon. 2/m :B2/m9.EC.20Suhailite(NH4)Fe2+3(AlSi3O10)(OH)2Mon. 2/m :B2/m9.EC.20EphesiteNaLiAl2(Al2Si2O10)(OH)2Tric. 1 :P19.EC.20NorrishiteKLiMn3+2(Si4O10)O2Mon. 2/m :B2/m9.EC.20PhlogopiteKMg3(AlSi3O10)(OH)2Mon. 2/m :B2/m9.EC.20YangzhumingiteKMg2.5(Si4O10)F2Mon. 2/m :B2/m9.EC.20OrloviteKLi2Ti(Si4O10)OFMon. 2 :B29.EC.20TetraferrianniteKFe2+3(Si3Fe3+)O10(OH)2Mon. 2/m :B2/m9.EC.20ShirokshiniteK(NaMg2)(Si4O10)F2Mon. 2/m :B2/m9.EC.20TrilithioniteK(Li1.5Al1.5)(AlSi3O10)(F,OH)2Mon. 2/m :B2/b9.EC.20PolylithioniteKLi2Al(Si4O10)(F,OH)2Mon. 2/m :B2/b9.EC.20ShirozuliteKMn2+3(Si3Al)O10(OH)2Mon. 2/m :B2/m9.EC.20PreiswerkiteNaMg2Al(Al2Si2O10)(OH)2Mon. 2/m :B2/b9.EC.20FluorophlogopiteKMg3(Si3Al)O10F2Mon. 2/m :B2/m9.EC.20Wonesite(Na,K)(Mg,Fe,Al)6((Al,Si)4O10)2(OH,F)4Mon. 2/m :B2/m9.EC.20UM2004-49-SiO:AlCsFHKLi(Cs,K)(Al,Li)2.6((Si,Al)4O10)(F,OH)29.EC.20FluorotetraferriphlogopiteKMg3(Fe3+Si3O10)F2Mon. 2/m :B2/m9.EC.20AnniteKFe2+3(AlSi3O10)(OH)2Mon. 2/m :B2/m9.EC.20EastoniteKMg2Al(Al2Si2O10)(OH)2Mon.9.EC.22PimeliteNi3Si4O10(OH)2 · 4H2OHex.9.EC.30MargariteCaAl2(Al2Si2O10)(OH)2Mon. 2/m :B2/b9.EC.30Chlorophaeite(Ca,Mg,Fe)2Fe2Si4O13 · 10H2O9.EC.35Kinoshitalite(Ba,K)(Mg,Mn2+,Al)3(Al2Si2O10)(OH)2Mon. 2/m :B2/m9.EC.35Ferrokinoshitalite(Ba,K)(Fe2+,Mg)3(Al2Si2O10)(OH,F)2Mon. 2/m :B2/m9.EC.35ClintoniteCaAlMg2(SiAl3O10)(OH)2Mon. 2/m :B2/m9.EC.35Oxykinoshitalite(Ba,K)(Mg,Ti,Fe3+,Fe2+)3((Si,Al)4O10)(O,OH,F)2Mon. 2/m :B2/m9.EC.35FluorokinoshitaliteBaMg3(Al2Si2O10)F2Mon. 2/m :B2/m9.EC.35BityiteCaLiAl2(AlBeSi2O10)(OH)2Mon. 2/m :B2/b9.EC.35Anandite(Ba,K)(Fe2+,Mg)3((Si,Al,Fe)4O10)(S,OH)2Mon. 2/m :B2/b9.EC.40Montmorillonite(Na,Ca)0.33(Al,Mg)2(Si4O10)(OH)2 · nH2OMon. 2/m :B2/m9.EC.40Beidellite(Na,Ca0.5)0.3Al2((Si,Al)4O10)(OH)2 · nH2OMon. 2/m :B2/m9.EC.40VolkonskoiteCa0.3(Cr,Mg,Fe)2((Si,Al)4O10)(OH)2 · 4H2OMon.9.EC.40NontroniteNa0.3Fe2((Si,Al)4O10)(OH)2 · nH2OMon. 2/m :B2/m9.EC.40Kurumsakite(Zn,Ni,Cu)8Al8V5+2Si5O35 · 27H2O (?)Orth.9.EC.40Yakhontovite(Ca,Na)0.5(Cu,Fe,Mg)2(Si4O10)(OH)2 · 3H2OMon.9.EC.45SwineforditeLi(Al,Li,Mg)3((Si,Al)4O10)2(OH,F)4 · nH2OMon. 2/m :B2/m9.EC.45HectoriteNa0.3(Mg,Li)3(Si4O10)(F,OH)2Mon. 2/m :B2/m9.EC.45ZincsiliteZn3Si4O10(OH)2 · 4H2O (?)Mon.9.EC.45HanjiangiteBa2CaV3+Al(H2AlSi3O12)(CO3)2FMon. 2 :B29.EC.45SpadaiteMgSiO2(OH)2 · H2O (?)9.EC.45FerrosaponiteCa0.3(Fe2+,Mg,Fe3+)3((Si,Al)4O10)(OH)2 · 4H2OMon.9.EC.45Stevensite(Ca,Na)xMg3-x(Si4O10)(OH)2Mon.9.EC.45SaponiteCa0.25(Mg,Fe)3((Si,Al)4O10)(OH)2 · nH2OMon.9.EC.45SauconiteNa0.3Zn3((Si,Al)4O10)(OH)2 · 4H2OMon.9.EC.50VermiculiteMg0.7(Mg,Fe,Al)6(Si,Al)8O20(OH)4 · 8H2OMon. 2/m9.EC.52Tarasovitenear NaKAl11Si13O40(OH)9 · 3H2O9.EC.55ClinochloreMg5Al(AlSi3O10)(OH)8Mon. 2/m :B2/m9.EC.55Borocookeite(LiAl4◻)[BSi3O10](OH)8Mon.m :Bb9.EC.55FranklinfurnaceiteCa2Fe3+Mn2+3Mn3+(Zn2Si2O10)(OH)8Mon. 2 :B29.EC.55PennantiteMn2+5Al(AlSi3O10)(OH)8Tric.9.EC.55Nimite(Ni,Mg,Al)6((Si,Al)4O10)(OH)8Mon. 2/m :B2/m9.EC.55Cookeite(LiAl4◻)[AlSi3O10](OH)8Mon. 2/m9.EC.55Gonyerite(Mn2+,Mg)5Fe3+(Fe3+Si3O10)(OH)8Orth.9.EC.55Chamosite(Fe2+,Mg,Al,Fe3+)6(Si,Al)4O10(OH,O)8Mon. 2/m :B2/m9.EC.55Orthochamosite(Fe2+,Mg,Fe3+)5Al(AlSi3O10)(OH,O)89.EC.55Baileychlore(Zn,Fe2+,Al,Mg)6(Si,Al)4O10(OH)8Tric.19.EC.55SudoiteMg2Al3(Si3Al)O10)(OH)8Mon. 2/m :B2/m9.EC.55GlagoleviteNa(Mg,Al)6(AlSi3O10)(OH,O)8Tric. 1 :P19.EC.55DonbassiteAl4.33(Si3Al)O10(OH)8Mon. 2 :B29.EC.60DozyiteMg7Al2(Al2Si4O15)(OH)12Mon.9.EC.60Rectorite(Na,Ca)Al4((Si,Al)8O20)(OH)4 · 2H2OMon.9.EC.60Corrensite(Mg,Fe)9((Si,Al)8O20)(OH)10 · nH2OOrth.9.EC.60AliettiteCa0.2Mg6((Si,Al)8O20)(OH)4 · 4H2OMon.9.EC.60Karpinskite(Ni,Mg)2Si2O5(OH)2 (?)Mon.9.EC.60LunijianlaiteLi0.7Al6.2(AlSi7O20)(OH,O)10Mon.9.EC.60TosuditeNa0.5(Al,Mg)6((Si,Al)8O18)(OH)12 · 5H2OMon. 2 :B29.EC.60HydrobiotiteK(Mg,Fe2+)6((Si,Al)8O20)(OH)4 · nH2OMon. 2/m :B2/m9.EC.60Saliotite(Li,Na)Al3(AlSi3O10)(OH)5Mon. 2/m :B2/m9.EC.60KulkeiteMg8Al(AlSi7O20)(OH)10Mon.9.EC.60BrinrobertsiteNa0.3Al4(Si4O10)2(OH)4 · 3.5 H2OMon.9.EC.65Macaulayite(Fe,Al)24Si4O43(OH)2Mon.9.EC.70BurckhardtitePb2(Fe3+Te6+)[AlSi3O8]O6Trig.3m(32/m) :P31m9.EC.75Niksergievite(Ba,Ca)2Al3(AlSi3O10)(CO3)(OH)6 · nH2OMon.9.EC.75Ferrisurite(Pb,Ca)2.4Fe3+2(Si4O10)(CO3)1.7(OH)3 · nH2OMon.9.EC.75Surite(Pb,Ca)3(Al,Fe2+,Mg)2((Si,Al)4O10)(CO3)2(OH)2Mon. 2 :P219.EC.80KegelitePb8Al4(Si8O20)(SO4)2(CO3)4(OH)8Mon.

Radioactivity

D = ((AU × ΓU) + (ATh × ΓTh) + (AK × ΓK)) / r2 × μshield

Other InformationQuartz-rich-coarse-grained-crystalline-rock
  • Granitoid
  • Fine-grained ("volcanic") normal crystalline igneous rock
  • Sedimentary rock and sediment
  • Metamorphic rock
  • Internet Links for Muscovite
    Search Engines:
  • Look for Muscovite on Google
  • Look for Muscovite images on Google
  • Look for Muscovite on Bing
  • Look for Muscovite images on Bing
  • Look for Muscovite on DuckDuckGo
  • Look for Muscovite images on DuckDuckGo
  • Look for Muscovite in the Rock H. Currier Digital Library
  • References for Muscovite
          • Réservoir-Dozois
    Olivier Langelier Collection
    Peru
     
    collections of Rock Currier+1 other reference
    Switzerland
     
    USA
     
    Solomon Feinstein Collection.+1 other reference[Phengite var: Mariposite]Bowen et al. (1957)+2 other referencesRon Layton CollectionCameron+7 other referencesRocks & Min 74:121 (1999)+1 other referenceLMSCC Newsletter+1 other referenceBowman (1902)+2 other references[var: Schernikite]Adam Berlutti collectionUSGS Professional Paper 255: 333-338.+2 other referencesJanuzzi et al. (1976)Anthony Scalzi collection[var: Illite]GSA Bulletin+3 other references[var: Schernikite]Cliff Trebilcock collection+1 other referenceK. Wood collection- (2005)Gordon (1922)Dana 6: 1088+5 other referencesF Roberts
     
    and/or 
    Mindat.org is an outreach project of theHudson Institute of Mineralogy, a 501(c)(3) not-for-profit organization.
    Copyright © mindat.org and the Hudson Institute of Mineralogy 1993-2025, except where stated. Most political location boundaries are© OpenStreetMap contributors. Mindat.org relies on the contributions of thousands of members and supporters. Founded in 2000 byJolyon Ralph.
    To cite: Ralph, J., Von Bargen, D., Martynov, P., Zhang, J., Que, X., Prabhu, A., Morrison, S. M., Li, W., Chen, W., & Ma, X. (2025). Mindat.org: The open access mineralogy database to accelerate data-intensive geoscience research. American Mineralogist, 110(6), 833–844.doi:10.2138/am-2024-9486.
    Privacy Policy -Terms & Conditions -Contact Us / DMCA issues -Report a bug/vulnerabilityCurrent server date and time: July 18, 2025 12:13:35 Page updated: July 18, 2025 00:49:28