Kozoite-(Nd)
Chemical formula: NdCO<sub>3</sub>(OH)
Kozoite-(Nd) is a rare mineral from the carbonate group, forming microscopic, spherulitic aggregates of a pinkish-violet color.
Properties
- Luster
- Vitreous
- Streak
- White
- Density
- 4.96
- Cleavage
- Perfect on {010}
- Transparency
- Transparent to translucent
- Crystal system
- Orthorhombic
Diagnostic features
## Identification Identification of kozoite-(Nd) is possible only through advanced laboratory methods, such as X-ray diffraction (XRD) and chemical microanalysis (e.g., EDS/WDS). Visually, it is practically impossible. Under laboratory conditions, its reaction with hydrochloric acid (HCl) is characteristic – it effervesces vigorously, which is typical for carbonates. ## Distinguishing from Similar Minerals It can be confused with other minerals from the ancylite group or other rare earth carbonates, such as bastnäsite or parisite. Differentiation requires specialized chemical analysis to determine the dominant rare earth element and analysis of the crystal structure. ## Crystal Forms It forms spherulitic (spherical) aggregates composed of radially arranged, lath-like or fibrous crystals. Individual, well-formed crystals are not observed.
Geological environment
## Genesis Kozoite-(Nd) is a secondary mineral, formed in the late stages of hydrothermal processes within syenite pegmatites. It forms in rock cavities and fissures as a result of alterations of earlier rare earth minerals. ## Mineral Associations This mineral occurs in association with other, often rare, minerals. In its type locality (Matsushiro, Japan), it was found in association with aegirine, microcline, quartz, eudialyte, as well as secondary minerals such as caysichite-(Y), kimuraite-(Y), lokkaite-(Y), bastnäsite-(Ce), and lanthanite-(Nd). ## Localities The only confirmed occurrence of kozoite-(Nd) in the world is its type locality – the Tenno quarry, located in Matsushiro, Ehime Prefecture, on Shikoku Island, Japan.
Rarity
Extremely rare
For collectors
## Quality Criteria The quality of kozoite-(Nd) specimens is primarily assessed based on the abundance and size of aggregates on the rock matrix. Since the mineral is microscopic, specimens where the spherulitic aggregates are numerous, well-formed, and visible under low magnification are most valued. Contrast with the matrix (e.g., dark aegirine) and the presence of rare associated minerals are also important. ## Popular Localities The only source of specimens is the Tenno quarry in Japan. Material from this locality is extremely difficult to obtain and appears on the collector's market sporadically.
Care and storage
## Cleaning Due to the extreme delicacy and microscopic size of the aggregates, mechanical cleaning is not recommended and can lead to the destruction of the specimen. If it is necessary to remove loose dust, compressed air can be used from a safe distance. ## What to Avoid Contact with acids, which rapidly decompose carbonates, should be strictly avoided. Avoid ultrasonics, steam cleaners, and all chemical agents. Protect from high temperatures, which can cause thermal decomposition of the mineral. ## Storage Kozoite-(Nd) specimens are usually very small and fragile, so they should be stored in stable conditions, in sealed "micromount" boxes, to protect them from mechanical damage, dust, and sudden changes in humidity.