Nioboixiolite-(Mn^2+^)
Chemical formula: (Nb<sup>5+</sup><sub>0.67</sub>Mn<sup>2+</sup><sub>0.33</sub>)O<sub>2</sub>
Nioboixiolite-(Mn²⁺) is a rare, black oxide mineral from the ixiolite group, containing niobium and manganese.
Properties
- Mohs hardness
- 6-6.5
- Luster
- Pitchy to submetallic
- Streak
- Black
- Density
- 5.91
- Cleavage
- Imperfect on {010}
- Fracture
- Uneven to conchoidal
- Transparency
- Opaque
- Crystal system
- Orthorhombic
Diagnostic features
## Identification Amateur identification of nioboixiolite-(Mn²⁺) is practically impossible. It requires advanced analytical methods, such as chemical composition analysis (EDS/WDS) and X-ray diffraction (XRD). It can be tentatively suspected based on its black color, resinous luster, high hardness and density, and occurrence in granitic pegmatites. ## Distinguishing from Similar Minerals This mineral is visually indistinguishable from other black, heavy pegmatite minerals, such as columbite, tantalite, wolframixiolite, or samarskite. Definitive differentiation is only possible through specialized laboratory tests. ## Crystal Forms It most often occurs as anhedral (undeveloped) grains or subhedral (poorly developed) prismatic crystals. Crystals are usually small, rarely exceeding a few millimeters.
Geological environment
## Genesis Nioboixiolite-(Mn²⁺) is a mineral of magmatic origin. It forms in the late stages of crystallization in complex granitic pegmatites, especially those enriched in lithium, cesium, and tantalum (LCT type). ## Mineral Associations It often co-occurs with other pegmatite minerals, such as quartz, albite, microcline, muscovite, lepidolite, as well as rarer niobium and tantalum minerals, e.g., columbite-(Mn), tantalite-(Mn), microlite, cassiterite, and beryl. ## Localities The most important and well-documented occurrences of this mineral worldwide include pegmatites in the Mâncio Lima region in Acre, Brazil; the Viitaniemi pegmatite in Finland; the Tanco Mine in Bernic Lake, Manitoba (Canada); and pegmatites in the Alto Ligonha region in Mozambique.
Rarity
Very rare
For collectors
## Quality Criteria The collector's appeal of a nioboixiolite-(Mn²⁺) specimen primarily depends on its documented provenance and analytically confirmed identity. Specimens with well-formed, even if partially, crystals are most valued. Association with other rare pegmatite minerals is also important, as it enhances the contextual value of the specimen. ## Popular Localities Specimens from classic localities, such as Viitaniemi in Finland or the Tanco Mine in Canada, are particularly sought after by specialized collectors due to their scientific and historical significance.
Care and storage
## Cleaning Specimens should only be cleaned mechanically, using a soft, dry brush or paintbrush to remove dust. Due to its rarity and potential co-occurrence with sensitive minerals, contact with water and chemical agents should be avoided. ## What to Avoid Ultrasonic cleaners and all acids and bases should be avoided, as they could damage the mineral's surface or associated minerals. It should not be heated or exposed to sudden temperature changes. ## Storage Nioboixiolite-(Mn²⁺) specimens are best stored in stable conditions, in a closed display box, to protect them from dust and mechanical damage. It is advisable to isolate it from other minerals to prevent scratching.