Jingwenite-(Y)

jingwenite-(Y)

xenotime-(Y)

thortveitite

nolanite

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Formula: YAlV4+(SiO4)O2(OH)2
Nesosilicate (insular SiO4 groups), yttrium- and vanadium- bearing mineral
Crystal System: Monoclinic
Specific gravity: 4.475 calculated
Hardness: 4½ to 5
Streak: yellowish grey
Colour: Light brown
Environments

Sedimentary

Jingwenite-(Y) is a new mineral, approved in 2021 and to date (January 2024) reported only from the type locality.

Localities

At the type lcality, the Yushui Mine, Mei county, Meizhou, Guangdong, China, jingwenite-(Y) is an abundant component of the sediment-hosted stratiform copper deposit. It occurs in bedded/massive sulphide-bearing ore and is associated with bornite, chalcopyrite, galena, xenotime-(Y), nolanite, thortveitite, roscoelite, baryte and quartz.
Jingwenite-(Y) is of epigenetic (formed later than the surrounding or underlying rock formation) origin and it appears that heavy rare earth elements and vanadium were added to the sediment-hosted stratiform copper system via leaching of abundant heavy minerals in the footwall red sandstone by oxidised basinal (pertining to a large low-lying area, often below sea level) brines. The abundance of jingwenite-(Y) at Yushui indicates that it could potentially be a valuable resource for heavy rare earth elements and vanadium (AM 108.192-196).

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