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Studenitsite


FieldValue
nameStudenitsite
categoryPhylloborates
imageStudenitsite.jpg
captionStudenitsite from the type and only known locality worldwide
formula
IMAsymbolSdn
molweight528 g/mol
strunz6.GB.05
systemMonoclinic
classPrismatic (2/m)
(same H-M symbol)
symmetryP21/c
unit cell,
; ;
colorColorless to light dirty-yellow and light grey
habitClusters of flattened wedge-shaped crystals
tenacityFragile
mohs5.5–6
lusterVitreous
refractive
opticalpropBiaxial (+)
birefringenceδ = 0.032
2VMeasured: 54°
streakWhite
gravity2.29
diaphaneityTransparent
otherNamed after Studenica, a cloister near the discovery locality.
references

(same H-M symbol) ; ; Studenitsite is a rare borate mineral with chemical formula of .

Studenitsite has a vitreous luster, a Mohs hardness of 6 and color of light-dirty yellow. The basic unit of the crystal structure layers has a Miller index of (001). Studenitsite has a low surface relief, which means the measure of the relative difference between the index of refraction of the mineral and surrounding medium is small. Birefringence is the difference between two principal indices of refraction of a uniaxial crystal. Studenitsite has a maximum birefringent value of . Studenitsite has three indices of refraction. Their values are , , . Indices of refraction are the ratio of the light's speed in the mineral and the medium.

Studenitsite is an extremely rare mineral that has only been found in the Piskaya deposit, Yarondolskii Basin, on the Ibar River, south of Belgrade, Serbia. The deposit is classified as a volcanogenic-sedimentary borate deposit with clay and carbonate minerals. It was named after the Studenica cloister near the discovery location.

References

References

  1. Warr, L.N.. (2021). "IMA–CNMNC approved mineral symbols". Mineralogical Magazine.
  2. "Studenitsite".
  3. (2014). "Lavendulan Mineral Data".
  4. (2005). "Studenitsite". Mineral Data Publishing.
  5. Jambor, L. John. (1996). "New Mineral Names". American Mineralogist.
  6. "Mineralienatlas - Fossilienatlas".
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