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   » » Wiki: Alabandite
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Alabandite or alabandine, formerly known as manganese blende or bluemenbachite is a rarely occurring . It crystallizes in the cubic crystal system with the chemical composition 2+ and develops commonly massive to granular aggregates, but rarely also cubic or octahedral crystals to 1 cm.


Etymology and history
Alabandite was first described in 1784 by Franz-Joseph Müller von Reichenstein. The mineral name is derived from its supposed discovery locality at (Aïdin) in Turkey.


Occurrence
Alabandite forms in polymetallic sulfide veins and low-temperature manganese deposits. It occurs with , , , , , , , , and native . Sometimes it was found in .

Localities are several areas in Antarctica, Argentina, Armenia, Australia, Bolivia, Brazil, Bulgaria, Canada, China, Czech Republic, Finland, France, Germany, Ghana, Greece, Greenland, India, Italy, Japan, Kyrgyzstan, Mexico, New Zealand, Norway, Peru, Poland, Romania, Russia, Slovakia, South Africa, South Korea, Sweden, Switzerland, Taiwan, Tanzania, the United Kingdom, the US, Uzbekistan and Yemen. All together at present time approximately 220 discovery sites are registered.


Crystal structure
Alabandite crystallizes in the cubic crystal system in the Fm3m with the a = 5.22 Å American Mineralogist Crystal Structure Database - Alabandite (1991) and four per unit cell.


See also
  • List of minerals

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