Lisiguangite is an exceptionally rare platinum-group sulfide mineral first identified in Chinese nickel-copper deposits. It typically forms as microscopic black metallic grains within complex sulfide matrices, making it a highly sought-after specimen for advanced mineral collectors.
Is this lisiguangite?
3-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 lisiguangite with a known reference. Lisiguangite sits at Mohs 2.5, softer than the next harder reference, harder than the previous one.
- 2Match the color rangeCompare against the expected color range: lead gray.
- 3Look at form & habitCrystal system: orthorhombic. Typical habit: euhedral crystals.
Often confused with
Lisiguangite vs. its common look-alikes, and how to tell them apart in the field.
Often found alongside lisiguangite
Minerals reported to co-occur with lisiguangite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- CuPtBiS₃
- Mohs hardness
- 2.5
- Density
- 7.42 g/cm³
- Colors
- Transparency
- Opaque
- Crystal system
- Orthorhombic
- Crystal habit
- Euhedral crystals
- Cleavage
- Perfect on {010}, distinct on {001}, visible on {100}
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Of contact metamorphic origin, along veins in an exoskarn associated with mafic igneous rocks (garnet pyroxenite)
Where rockhounds find lisiguangite
Classic worldwide localities
- Sandao Village, 250 km northeast of Beijing, Yanshan Mountains, Hebei Province, China
Field-hunting tip
Where it forms: Of contact metamorphic origin, along veins in an exoskarn associated with mafic igneous rocks (garnet pyroxenite). If you start seeing bornite, galena, carrolite in float, you are in the right ground. Typical habit: euhedral crystals. Train your eye for that shape before scanning the outcrop.







