Jump to content
 







Main menu
   


Navigation  



Main page
Contents
Current events
Random article
About Wikipedia
Contact us
Donate
 




Contribute  



Help
Learn to edit
Community portal
Recent changes
Upload file
 








Search  

































Create account

Log in
 









Create account
 Log in
 




Pages for logged out editors learn more  



Contributions
Talk
 



















Contents

   



(Top)
 


1 Description  





2 History  





3 Occurrence and distribution  





4 References  



4.1  Bibliography  







5 Further reading  





6 External links  














Serandite






Авар
Català
Deutsch
Español
Esperanto
Euskara
Français
Italiano
Norsk nynorsk
Русский
Українська

 

Edit links
 









Article
Talk
 

















Read
Edit
View history
 








Tools
   


Actions  



Read
Edit
View history
 




General  



What links here
Related changes
Upload file
Special pages
Permanent link
Page information
Cite this page
Get shortened URL
Download QR code
Wikidata item
 




Print/export  



Download as PDF
Printable version
 




In other projects  



Wikimedia Commons
 
















Appearance
   

 






From Wikipedia, the free encyclopedia
 


Serandite
Serandite from Mont Saint-Hilaire, Quebec, Canada
General
CategoryInosilicates
Formula
(repeating unit)
Na(Mn2+,Ca)2Si3O8(OH)
IMA symbolSrd[1]
Strunz classification9.DG.05
Dana classification65.2.1.5
Crystal systemTriclinic
Crystal classPinacoidal (1)
(same H-M symbol)
Space groupP1
Unit cella = 7.683(1Å, b = 6.889(1) Å
c = 6.747(1) Å, α = 90.53(5
β = 94.12(2)°, γ = 102.75(2
Z = 2
Identification
Coloursalmon pink to orange
TwinningAround [010] composition plane {100}, less commonly contact twin on {110}
CleavagePerfect on {001} and {100}
FractureIrregular, uneven
TenacityBrittle
Mohs scale hardness5 to 5.5
LusterVitreous to greasy; fibrous aggregates are dull to silky[2]
StreakWhite
DiaphaneityTransparent, Translucent
Density3.34 g/cm3 (measured)
Optical propertiesBiaxial (+)
Refractive indexnα = 1.668
nβ = 1.671
nγ = 1.703
Birefringenceδ = 0.035
2V angle39°
Dispersionr < v moderate
References[3]

Serandite[4] is a mineral with formula Na(Mn2+,Ca)2Si3O8(OH). The mineral was discovered in Guinea in 1931 and named for J. M. Sérand. Serandite is generally red, brown, black or colorless. The correct name lacks an accent.[5]

Description

[edit]

Serandite is transparent to translucent and is normally salmon-pink, light pink, rose-red, orange, brown, black, or colorless; in thin section, it is colorless.[2] Octahedrally bonded Mn(II) is the primary contributor to the mineral's pink colors.[6]

Crystals of the mineral can be prismatic to acicular and elongated along [010], bladed, blocky, or tabular and flattened on {100}, occur as a radiating aggregate, or have massive habit.[2] Sérandite is a member of the wollastonite group and is the manganese analogue of pectolite.[3] It is sometimes used as a gemstone.[7]

History

[edit]

Serandite was discovered on Rouma Island, part of the Los Islands in Guinea.[3] The mineral was described by À. Lacroix in the journal Comptes rendus hebdomadaires des séances de l'Académie des Sciences.[8] He named it sérandite in honor of J.M. Sérand, a mineral collector who helped in the collection of the mineral.[3]

Occurrence and distribution

[edit]

Serandite has been found in Australia, Brazil, Canada, Guinea, Italy, Japan, Namibia, Norway, Russia, South Africa, and the United States.[3] The type material is held at the National Museum of Natural History in Washington, D.C.[2]

AtMont Saint-Hilaire, Quebec, serandite occurs in sodalite xenoliths and pegmatites cutting syenites within an intrusive alkalic gabbro-syenite complex. In Point of Rocks, New Mexico, it occurs in vugsinphonolite. At the Tumannoe deposit in Russia, serandite occurs in a manganese rich deposit associated with volcanic rocks and terrigenous (non-marine) sediments which has been altered by contact metamorphism.[2]

Serandite has been found in association with aegirine, analcime, arfvedsonite, astrophyllite, eudialyte, fluorite, leucophanite, mangan-neptunite, microcline, nepheline, sodalite, and villiaumite.[2]

References

[edit]
  1. ^ Warr, L.N. (2021). "IMA–CNMNC approved mineral symbols". Mineralogical Magazine. 85 (3): 291–320. Bibcode:2021MinM...85..291W. doi:10.1180/mgm.2021.43. S2CID 235729616.
  • ^ a b c d e f "Sérandite" (PDF). Handbook of Mineralogy. Mineral Data Publishing. Archived from the original (PDF) on September 11, 2021. Retrieved July 11, 2012.
  • ^ a b c d e "Sérandite". Mindat. Retrieved July 11, 2012.
  • ^ "Serandite". Webmineral. Retrieved July 25, 2012.
  • ^ Hålenius, U., Hatert, F., Pasero, M., and Mills, S.J., IMA Commission on New Minerals, Nomenclature and Classification (CNMNC) Newsletter 28. Mineralogical Magazine 79(7), 1859–1864
  • ^ Manning, p. 357.
  • ^ Gemstones of North America – Volume 3 – Page 417 John Sinkankas – 1959
  • ^ Lacroix, p. 189.
  • Bibliography

    [edit]

    Further reading

    [edit]
    [edit]

    Media related to Serandite at Wikimedia Commons


    Retrieved from "https://en.wikipedia.org/w/index.php?title=Serandite&oldid=1196954641"

    Categories: 
    Triclinic minerals
    Sodium minerals
    Manganese(II) minerals
    Calcium minerals
    Hydroxide minerals
    Inosilicates
    Gemstones
    Minerals in space group 2
    Hidden categories: 
    Articles with short description
    Short description is different from Wikidata
    CS1 French-language sources (fr)
    Commons category link is on Wikidata
     



    This page was last edited on 18 January 2024, at 23:39 (UTC).

    Text is available under the Creative Commons Attribution-ShareAlike License 4.0; additional terms may apply. By using this site, you agree to the Terms of Use and Privacy Policy. Wikipedia® is a registered trademark of the Wikimedia Foundation, Inc., a non-profit organization.



    Privacy policy

    About Wikipedia

    Disclaimers

    Contact Wikipedia

    Code of Conduct

    Developers

    Statistics

    Cookie statement

    Mobile view



    Wikimedia Foundation
    Powered by MediaWiki