Orthobrannerite

Chemical formula: U₄+U₆+Ti₄+₄O₁₂(OH)₂

Orthobrannerite is an extremely rare, radioactive uranium and titanium mineral, forming microscopic, black crystals in pegmatites.

## Characteristics Orthobrannerite is an oxide of uranium and titanium, belonging to rare minerals. It occurs as very small, prismatic crystals, rarely exceeding 0.5 mm in length. These crystals often form radial or stellate aggregates. The mineral is black and opaque. ## Physical Properties It is characterized by a luster described as submetallic to greasy. Its density is approximately 5.35 g/cm³. The Mohs hardness has not been precisely determined. The mineral does not exhibit cleavage, and its fracture is conchoidal. The streak is black. As a uranium mineral, orthobrannerite is strongly radioactive. ## Colors and Varieties Orthobrannerite is known exclusively in black. No color or commercial varieties are distinguished. ## History and Name The mineral was first described in 1984 by T.T. Chen and co-workers. Its name refers to its orthorhombic crystal system and its chemical and structural similarity to brannerite. ## Applications Due to its extreme rarity, orthobrannerite has no industrial application. It is solely an object of scientific interest and is valued by specialized collectors of rare minerals and radioactive minerals.

Properties

Luster: Submetallic to greasy
Streak: Black
Density: 5.35
Cleavage: None
Fracture: Conchoidal
Transparency: Opaque
Crystal system: Orthorhombic

Diagnostic features

## Identification The key diagnostic feature of orthobrannerite is its strong radioactivity, easily detectable with a Geiger counter. Visually, it is recognized by its black color, submetallic luster, and typical radial aggregates of small, prismatic crystals. ## Distinguishing from similar minerals Orthobrannerite can be confused with brannerite, uraninite, or other black, radioactive minerals. It is distinguished from brannerite, which crystallizes in the monoclinic system, by its orthorhombic crystal symmetry. Uraninite usually forms isometric (cubic) crystals and has a different chemical composition. Definitive differentiation requires advanced analytical methods, such as X-ray diffraction (XRD). ## Crystal forms It forms short, prismatic crystals, most often occurring as small, radial or stellate aggregates.

Geological environment

## Genesis Orthobrannerite is a secondary mineral, forming in the oxidation zones of uranium deposits. Its occurrence is closely associated with granitic pegmatites. ## Mineral associations It most often co-occurs with quartz, potassium feldspars, uraninite, and brannerite. ## Localities The only confirmed and typical locality (type locality) of orthobrannerite is the Nopal I uranium deposit in the Sierra Peña Blanca region in Chihuahua, Mexico. This is the only source of specimens of this mineral in the world.

Rarity

Extremely rare

For collectors

## Quality criteria The quality of orthobrannerite specimens, which are almost exclusively micromounts, is assessed based on the sharpness and development of crystals within the aggregate. Specimens with distinct, radial groupings on a contrasting substrate (matrix) are most valued. Due to the microscopic size of the crystals, their size is less important than the form and richness of the aggregate. ## Popular localities All known collector specimens come from a single location in the world: the Nopal I deposit in Mexico. This makes the mineral extremely desirable among collectors specializing in rare species or minerals from specific localities.

Care and storage

## Cleaning Orthobrannerite specimens, usually in the form of micromounts, generally do not require cleaning. If dust needs to be removed, compressed air can be used. Avoid contact with water and chemical agents. ## What to avoid The mineral is strongly radioactive. Avoid direct, prolonged contact, and especially inhalation of dust and particles. Store away from minerals that may be damaged by radiation (e.g., some fluorites, smoky quartz). It should not be heated. ## Storage Specimens must be stored in specialized, lead-lined containers, clearly marked with the radioactivity symbol. Containers should be kept in an area isolated from living spaces and away from other specimens in the collection.

Sources

IMA Mineral List (CNMNC)