Shenzhuangite is an extremely rare iron-nickel sulfide mineral typically found in meteorites. It occurs as microscopic anhedral grains, most commonly identified during advanced geochemical analysis of meteoritic samples.
Is this shenzhuangite?
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 shenzhuangite with a known reference. Shenzhuangite 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. Shenzhuangite leaves a black streak.
- 3Read the lusterHold the specimen under a strong light. Shenzhuangite typically shows a metallic luster.
- 4Match the color rangeCompare against the expected color range: white, pale yellow.
- 5Look at form & habitCrystal system: cubic. Typical habit: anhedral grains.
Often confused with
Shenzhuangite vs. its common look-alikes, and how to tell them apart in the field.

How to tell apart: Streak differs, so Shenzhuangite leaves black, Pentlandite leaves light bronze-brown.

How to tell apart: Pyrite is the harder of the two (Mohs 6-6.5 vs. 3.5-4); streak differs, so Shenzhuangite leaves black, Pyrite leaves greenish-black to brownish-black.
Often found alongside shenzhuangite
Minerals reported to co-occur with shenzhuangite. Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- FeNiS₂
- Mohs hardness
- 3.5-4
- Density
- 6.12 g/cm³
- Colors
- Streak
- Black
- Luster
- Metallic
- Transparency
- Opaque
- Crystal system
- Cubic
- Crystal habit
- Anhedral Grains
- Cleavage
- None
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Meteorites
Where rockhounds find shenzhuangite
Classic worldwide localities
- Shenzhuang, China
- various meteorites
Field-hunting tip
Look in meteorites country, the host setting where shenzhuangite typically forms. If you start seeing troilite, kamacite, taenite in float, you are in the right ground. Field specimens usually show a anhedral grains habit, so train your eye for that shape before scanning the outcrop.


