- Chemistry: Ca(Ce, La, Nd)2(CO3)3F2 , Calcium Cerium Lanthanum Neodymium Carbonate Fluoride.
- Class: Carbonates
- Groups: Rare earth carbonates and Bastnasite.
- Uses: As a minor ore of cerium and other rare earth metals and as mineral specimens.
Parisite, which is named for the owner of the mine (J.J. Paris) at which parisite was discovered, is one of a
few rare earth carbonate minerals.
Some of the other more common rare earth carbonates are
Parisite has cerium, neodymium and lanthanum in its generalized formula but officially the mineral is divided into two minerals based on the respective predominant rare earth element.
There is the more common parisite-(Ce) with a more accurate formula of Ca(Ce, La)2(CO3)3F2.
And there is the rarer parisite-(Nd) with a formula of Ca(Nd, Ce, La)2(CO3)3F2.
There is little difference in the two in terms of physical properties and most Parisite is actually Parisite-(Ce).
Parisite is closely related to three other distinct minerals;
The four are all Bastnasite Group minerals of similar formulas and occurrence.
In Fact the four are often intergrown and a single crystal of any of these minerals probably contains at least one of the other minerals and possibly all four.
As expected they can be difficult to distinguish from one another.
One unique method involves the dissolvability of the four minerals in acids.
Bastnasite is nearly indissolvable in cold nitric acid followed by parisite's slow dissolution, while rontgenite readily dissolves and synchysite dissolves the quickest.
With a practiced hand, identification of samples can be made by gauging the rates of dissolution.
Differing dissolution rates within a single crystal can also confirm the multiple phases or species that exist within the crystal, but this also tends to ruin the specimen.
The zoning of different phases is not generally visible in untested specimens.
Crystals often will show a zoning of inclusions but these do not indicate the boundaries of phases.
Parisite is only found as small crystals and can be used for micromounts.
Some crystals have been reported to have been cut as gems, but normally the crystals of parisite are too small and cloudy to make good gemstones.
Parisite crystals are found in carbonatites, granite pegmatites and alkaline syenites and the hydrothermal deposits associated with them.
Parisite is a significant ore at the bastnasite mines of Mountain Pass, California.
- Color is white, tan, yellow-brown, reddish-brown, brown, yellow and pale pink.
- Luster is vitreous, resinous to dull.
- Transparency: Crystals are translucent to more rarely transparent.
- Crystal System is trigonal.
- Crystal Habits include small acicular, platy or thin tabular crystals that form rosettes.
Also known to form double hexagonal pyramids and rhombohedrons.
Often intergrown in a lamellar fashion with synchysite, rontgenite and bastnasite.
- Cleavage is fair to good in one direction (basal).
- Fracture is subconchoidal to splintery.
- Hardness is typically around 4.5 but will vary from 4 to 5.
- Specific Gravity is approximately 4.2 to 4.3 (well above average)
- Streak is white to yellowish white.
- Other Characteristics: Only slightly soluble in nitric acid, a strong basal parting is also sometimes seen and crystals are typically striated parallel to the basal face.
- Associated Minerals are extensive and include
monazite and xenotime.
- Notable Occurrences include the type locality in the Muzo emerald deposit in the Muzo district, Bogota, Colombia.
Other localities include the Mountain Pass, San Bernardino, California; Quincy, Mass.; Mohave County, Arizona and Mineral and Ravelli Counties, Montana, USA;
the mines of Mont Saint-Hilaire, St. Honore and Gatineau, Quebec and the Thor Lake deposits, Northwest Territories, Canada;
langesundsfjord area, Norway and the
Weishan deposit, Weishan Lake district, Shandong Province, China
and the type locality for parisite-(Nd) that being Bayan Obo, inner Mongolia, China.
- Best Field Indicators: crystal habit, color, cleavage, density, luster, low solubility in nitric acid and locality.