Tenorite

Not to be confused with Tannerite.
Tenorite

A sample of tenorite
General
Category Oxide mineral
Formula
(repeating unit)		 CuO
Strunz classification 4.AB.10
Crystal system Monoclinic
Unit cell a = 4.6837(5) Å
b = 3.4226(5) Å
c = 5.1288(6) Å; β = 99.47°; Z = 4
Identification
Color Steel-gray, iron-gray, black
Crystal habit Lathlike crystals, curved, scaly, dendritic; commonly pulverulent, earthy, massive
Crystal symmetry Monoclinic - prismatic
H-M symbol: (2/m)
Space group: C 2/c
Twinning Common on {011}, forming stellate groups; lamellar
Cleavage Poor to indistinct
Fracture Conchoidal to uneven
Tenacity Brittle; flexible and elastic in thin scales
Mohs scale hardness 3.5 - 4
Luster Metallic to earthy
Streak Black
Diaphaneity Opaque, thin flakes transparent
Specific gravity 6.5
Optical properties Biaxial +
Pleochroism Distinct; light to dark brown
References [1][2][3]

Tenorite is a copper oxide mineral with the simple formula CuO.

Occurrence

Tenorite with azurite from Nischne Tagilsk, Urals, Russia

Tenorite occurs in the weathered or oxidized zone associated with deeper primary copper sulfide orebodies. Tenorite commonly occurs with chrysocolla and the copper carbonates, azurite and malachite. The dull grey-black color of tenorite contrasts sharply with the often intergrown blue chrysocolla. Cuprite, native copper and Fe–Mn oxides also occur in this environment.[1]

In addition to the hydrothermal, tenorite also occurs as a volcanic sublimate from Vesuvius, Campania, and Etna, Sicily, Italy. As a sublimate it occurs with copper chlorides, alkali chlorides and cotunnite.[1] The Vesuvian sublimate occurrence was originally named melaconise or melaconite by F. S. Beudant in 1832.[4]

Tenorite was named in 1841 after the Italian botanist Michele Tenore (1780-1861).[3]

See also

References

  1. 1 2 3 Handbook of Mineralogy
  2. ↑ Webmineral data
  3. 1 2 Mindat
  4. ↑ Chisholm, Hugh, ed. (1911). Encyclopædia Britannica (11th ed.). Cambridge University Press
This article is issued from Wikipedia - version of the Tuesday, April 05, 2016. The text is available under the Creative Commons Attribution/Share Alike but additional terms may apply for the media files.