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Keystoneite

From Wikipedia, the free encyclopedia
Keystoneite
General
CategoryTellurite minerals
GroupZemannite group
FormulaMg0.5Ni2+Fe3+(Te4+O3)3 · 4.5H2O
IMA symbolKys
IMA statusApproved
Strunz classification4.JM.05
Dana classification34.3.2.3
Crystal systemHexagonal
Crystal classHexagonal pyramidal (6)
Space groupP63 (no. 173)
Identification
ColorGolden yellow
LustreAdamantine
StreakPale yellow-green
DiaphaneityTranslucent
Specific gravity4.4
Density4.4 g/cm3
References[1]

Keystoneite is a naturally occurring tellurite mineral. It was discovered in 1988 at Keystone mine, Colorado, the type locality for which it is named.[1][2] It is the Ni2+ analogue of zemannite.[3][4]

References

[edit]
  1. 1 2 "Keystoneite". www.mindat.org. Retrieved 2026-03-07.
  2. "Keystoneite Mineral Data". webmineral.com. Retrieved 2026-03-17.
  3. Keystoneite (PDF), Mineral Data Publishing
  4. Missen, Owen P.; Back, Malcolm E.; Mills, Stuart J.; Roberts, Andrew C.; LePage, Yvon; Pinch, William W.; Mandarino, Joseph A. (March 1, 2021). "Crystal Chemistry of Zemannite-Type Structures: III. Keystoneite, the Ni2+-Analogue of Zemannite, and Ferrotellurite Discredited". The Canadian Mineralogist. 59 (2): 355–364. doi:10.3749/canmin.2000009. ISSN 1499-1276.