Dingdaohengite-(Ce) is a rare mineral belonging to the perrierite group, typically occurring in complex carbonatite-hosted environments. It is characterized by its dark, often tabular crystals and submetallic luster. It is primarily sought after by advanced systematic mineral collectors due to its restricted occurrence at the Bayan Obo deposit.
Is this dingdaohengite-(ce)?
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 dingdaohengite-(ce) with a known reference. Dingdaohengite-(Ce) sits at Mohs 5-6 — softer than the next harder reference, harder than the previous one.
- 2Check the streakDrag the specimen across an unglazed porcelain plate. Dingdaohengite-(Ce) leaves a greyish-brown streak.
- 3Read the lusterHold the specimen under a strong light. Dingdaohengite-(Ce) typically shows a submetallic luster.
- 4Match the color rangeCompare against the expected color range: black, brown.
- 5Look at form & habitCrystal system: monoclinic. Typical habit: tabular crystals.
Often confused with
Dingdaohengite-(Ce) vs. its common look-alikes — and how to tell them apart in the field.
Often found alongside dingdaohengite-(ce)
Minerals reported to co-occur with dingdaohengite-(ce). Spotting these in float or country rock is a strong cue you are in the right ground.
All properties
- Chemical formula
- (Ce,Ca,Sr,Na)₄(Fe²⁺,Mg,Mn)₂(Ti,Fe³⁺)₃Si₄O₂₂
- Mohs hardness
- 5-6
- Density
- 4.6-4.8 g/cm³
- Streak
- Greyish-brown
- Luster
- Submetallic
- Transparency
- Opaque
- Crystal system
- Monoclinic
- Crystal habit
- Tabular Crystals
- Cleavage
- None
- Rarity
- Rare
- Uses
- Collector
- Host rock
- Hydrothermal Veins in Carbonatite Deposits
- Typical price
- $50-300+ depending on specimen quality
Where rockhounds find dingdaohengite-(ce)
Classic worldwide localities
- Bayan Obo, Inner Mongolia, China
Field-hunting tip
Look in hydrothermal veins in carbonatite deposits country — that is the host setting where dingdaohengite-(ce) typically forms. If you start seeing aegirine, baryte, fluorite in float, you are in the right ground. Field specimens usually show a tabular crystals habit, so train your eye for that shape before scanning the outcrop.





