Mianningite is a rare, complex uranium-bearing oxide mineral discovered in the Maoniuping carbonatite deposit in Sichuan, China. It is typically found as dark, submetallic grains associated with rare-earth element minerals and must be handled with appropriate radiation safety precautions due to its uranium content.
Is this mianningite?
5-step field checkRun through these checks against the specimen in your hand. The more boxes tick, the more confident the ID.
- 1Test the hardnessTry to scratch mianningite with a known reference. Mianningite sits at Mohs ~6, softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Streak: black.
- 3Read the lusterHold the specimen under a strong light. Luster: submetallic.
- 4Match the color rangeCompare against the expected color range: black.
- 5Look at form & habitCrystal system: trigonal. Typical habit: anhedral to subhedral grains.
Often confused with
Mianningite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside mianningite
Minerals reported to co-occur with mianningite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- (□,Pb,Ce,Na)(U,Mn,U)Fe₂(Ti,Fe)₁₈O₃₈
- Mohs hardness
- ~6
- Density
- 4.62 g/cm³
- Colors
- Streak
- Black
- Luster
- Submetallic
- Transparency
- Opaque
- Crystal system
- Trigonal
- Crystal habit
- Anhedral to subhedral grains
- Cleavage
- None
- Rarity
- Rare
- Uses
- Collector
- Host rock
- In fractures within lamprophyre veins and their contacts with a later quartz-alkali feldspar syenite dike containing REE, U, and Th mineralization
Where rockhounds find mianningite
Classic worldwide localities
- Baozi Hill, near the Maoniuping REE mine, Mianning county, Sichuan province, China
Field-hunting tip
Where it forms: In fractures within lamprophyre veins and their contacts with a later quartz-alkali feldspar syenite dike containing REE, U, and Th mineralization. If you start seeing microcline, albite, quartz in float, you are in the right ground. Typical habit: anhedral to subhedral grains. Train your eye for that shape before scanning the outcrop.







