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Kyawthuite
Oxide mineral From Wikipedia, the free encyclopedia
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Kyawthuite (/ˈtʃɜːrˌtuːaɪt/)[4] is a rare mineral[2] with formula BiSbO4.[3] It is a natural bismuth antimonate, in which bismuth has oxidation state +3, and antimony oxidation state +5.[5]
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Description
Kyawthuite is monoclinic, with space group I2/c, and is isostructural with clinocervantite,[2] its trivalent-antimony-analogue.[6] Kyawthuite is an antimony-analogue of clinobisvanite.[7]
Occurrence
Kyawthuite was discovered in the vicinity of Mogok in Myanmar, an area famous for its variety of gemstone minerals,[8] in 2010 and was subsequently identified as being a new specimen by Dr. Kyaw Thu. The International Mineralogical Association officially recognised kyawthuite as a new mineral in 2015.[9]
Only one 0.3-gram sample of the naturally occurring form of this mineral is documented, and it is stored and on display at the Natural History Museum of Los Angeles County.[10] [11]

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References
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