Luobusaite is a rare iron silicide mineral first discovered in the Luobusa ophiolite of Tibet. It is typically found as microscopic grains or small aggregates embedded within chromite and peridotite, requiring advanced analytical techniques for positive identification in most cases.
Is this luobusaite?
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 luobusaite with a known reference. Luobusaite sits at Mohs 3.5-4 — softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Luobusaite leaves a black streak.
- 3Read the lusterHold the specimen under a strong light. Luobusaite typically shows a metallic luster.
- 4Match the color rangeCompare against the expected color range: white, gray, silver-white.
- 5Look at form & habitCrystal system: hexagonal. Typical habit: granular, irregular grains.
Often confused with
Luobusaite vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside luobusaite
Minerals reported to co-occur with luobusaite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- Fe₃Si₇
- Mohs hardness
- 3.5-4
- Density
- 6.8-7.2 g/cm³
- Colors
- Streak
- Black
- Luster
- Metallic
- Transparency
- Opaque
- Crystal system
- Hexagonal
- Crystal habit
- Granular, Irregular Grains
- Cleavage
- None
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Ophiolitic Peridotite
- Typical price
- $50-500 depending on specimen size and rarity
Where rockhounds find luobusaite
Classic worldwide localities
- Luobusa Ophiolite, Tibet, China
Field-hunting tip
Look in ophiolitic peridotite country — that is the host setting where luobusaite typically forms. If you start seeing chromite, olivine, diamond in float, you are in the right ground. Field specimens usually show a granular, irregular grains habit, so train your eye for that shape before scanning the outcrop.






