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Tuyamunit

Tyuyamunit is a radioactive mineral of the group of uranium mica . It is a calcium analogue of carnotite . It is described by K. A. Nenadkenich in 1912 , as a new mineral from the Tyuya-Muyun deposit ( Kyrgyzstan ).

Tuyamunit
Tyuyamunite-286294.jpg
FormulaCa [UO 2 ] [V 2 O 8 ] x 8H 2 O
Physical properties
Colourcanary yellow, lemon yellow, greenish yellow
Color featuresyellow
Shinediamond, waxy, pearly, dull
Transparencytranslucent, opaque
Hardness1.5—2
Cleavagevery perfect in {001}, mica-like; clear by {100} and {010}
Kinkmica-like
Density3.57-4.35 g / cm³
SyngonyRhombic , orthorhombic

Content

Description

The crystalline structure is layered. Syngonia is rhombic. Cleavage is perfect. The appearance is lamellar. Color is yellow with an orange-yellow or greenish tint. Gloss mother-of-pearl or glass. It occurs in the form of scales, or in the form of powder clusters. The break is mica-like.

Location

It occurs in sedimentary rocks when exposed to bicarbonate water on carnotite.

Literature

  • Nenadkevich K. A. Results of a study of the Tyuya-Muyun uranium and vanadium mine in the Ferghana region // Notes of St. Petersburg. Mineralogical Society. 1909. Ser. 2. Part 47. Protocols. S. 839.
  • Nenadkevich K. A. Tuyamunit - a new mineral species // Proceedings of the Imperial Academy of Sciences. 1912. Ser. 6. No. 15. P. 945–946.
  • Nenadkevich K.A., Volchkov P.A. On a new mineral - Tangeit from Tuyamuyun // Dokl. Academy of Sciences of the USSR. Ser. A. 1926. March. C. 43-46.

Links

  • [1] Tuyamunit at Geowiki


Source - https://ru.wikipedia.org/w/index.php?title= Tuyamunit&oldid = 86213965


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