Miessiite
Chemical formula: Pd<sub>11</sub>Te<sub>2</sub>Se<sub>2</sub>
Miessiite is a very rare palladium telluride and selenide, forming microscopic, metallic grains in association with other platinum-group minerals.
Properties
- Luster
- Metallic
- Density
- 10.85
- Transparency
- Opaque
- Crystal system
- Orthorhombic
Diagnostic features
## Identification Identification of miessiite is impossible without advanced laboratory techniques. In reflected light under a polarizing microscope, it exhibits a creamy-white color, weak pleochroism, and distinct anisotropy. Final confirmation requires chemical composition analysis (e.g., using an electron microprobe - EDS/WDS) and X-ray diffraction (XRD) studies. ## Distinguishing from similar minerals Miessiite is visually almost identical to other rare palladium minerals, such as keithconnite, telargpalite, kotulskite, or merenskyite, with which it often coexists. Differentiation is possible only based on a precise analysis of the palladium, tellurium, and selenium ratio in its chemical composition. ## Crystal forms Miessiite forms microscopic, elongated or lamellar crystals up to 60 x 15 μm in size. It occurs as single grains or in intergrowths with other platinum-group minerals.
Geological environment
## Genesis Miessiite forms as a result of hydrothermal processes within ultramafic rocks (komatiites). It crystallizes in zones enriched in platinum-group elements (PGE), from solutions rich in palladium, tellurium, and selenium. ## Mineral associations This mineral coexists with other platinum-group minerals (PGM), such as keithconnite, kotulskite, merenskyite, palladoarsenide, palladobismutoarsenide, as well as chalcopyrite, pentlandite, pyrite, chromite, and native gold. ## Localities The only confirmed and described locality of miessiite in the world is its discovery site - the Miessi gold mine in Inari, Finnish Lapland.
Rarity
Extremely rare
For collectors
## Quality criteria The quality of a miessiite specimen is determined solely by its scientific and documentary value. Since the mineral is invisible to the naked eye, collector specimens are fragments of host rock in which the presence of miessiite has been analytically confirmed. The most valuable are samples from the type locality (topotypes), rich in intergrowths with other rare PGM minerals. ## Popular localities The only source of specimens is the Miessi mine in Finland. Material from this locality is extremely difficult to obtain and is available almost exclusively in institutional collections and from specialized micromineral collectors.
Care and storage
## Cleaning Specimens containing miessiite, which are typically fragments of host rock, should not be wet cleaned. The safest method is to remove dust using compressed air or a very soft brush, with the utmost care. ## What to avoid Avoid contact with any chemicals, acids, and detergents. Due to its chemical composition, it may react with strong oxidizers. It should be protected from moisture and extreme temperatures. ## Storage Specimens containing miessiite should be stored in stable conditions, preferably in sealed "micromount" boxes, which protect them from dust, moisture, and mechanical damage. Avoid exposure to direct sunlight.