Keystoneite
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Keystoneite is a naturally occurring tellurite mineral. It was discovered in 1988 at Keystone mine, Colorado, the type locality for which it is named. It is the Ni 2+ analogue of zemannite.
Keystoneite is a naturally occurring tellurite mineral. It was discovered in 1988 at Keystone mine, Colorado, the type locality for which it is named. It is the Ni 2+ analogue of zemannite.
References
Text derived from https://en.wikipedia.org/w/index.php?oldid=1354356883 under CC BY-SA 4.0; modifications have been made.