Clino-oscarkempffite

Chemical formula: Ag¹⁺₁₅Pb²⁺₆Sb³⁺₂₁Bi³⁺₁₈S²⁻₇₂

A rare sulfosalt of lead, silver, antimony, and bismuth, forming acicular crystals with a metallic luster.

## Characteristics Clino-oscarkempffite is a complex sulfosalt belonging to the lillianite series. It occurs as elongated, acicular or bladed crystals, which can form tangled aggregates. Its color is grayish-black, and on fresh fracture surfaces, it exhibits a metallic luster. It is an opaque mineral. ## Physical Properties This mineral is characterized by a hardness of 3-3.5 on the Mohs scale, making it relatively soft. Its density is significant, approximately 6.04 g/cm³, which is typical for minerals containing heavy metals such as lead and bismuth. The fracture is uneven. ## History and Name Clino-oscarkempffite was described as a new mineral in 2018. Its name honors Professor Oscar Kempff, a Bolivian mineralogist and deposit researcher, for his contributions to the understanding of Bolivian mineralogy. The prefix "clino-" refers to its monoclinic crystallographic symmetry.

Properties

Mohs hardness
3-3.5
Luster
Metallic
Streak
Dark grey
Density
6.04
Fracture
Irregular/Uneven
Transparency
Opaque
Crystal system
Monoclinic

Diagnostic features

## Identification Characteristic features include acicular crystal habit, grayish-black color, metallic luster, and a dark gray streak. High density is also an important indicator. However, final identification requires advanced analytical methods, such as chemical composition analysis (EDS) and X-ray diffraction (XRD). ## Distinguishing from Similar Minerals It can be confused with other acicular sulfosalts, such as jamesonite, boulangerite, or other minerals from the lillianite group. Differentiation by eye is practically impossible and requires specialized laboratory equipment to confirm the presence and proportions of silver, lead, antimony, and bismuth. ## Crystal Forms It forms prismatic, acicular crystals, elongated along one axis. These crystals often occur as tangled or radial aggregates.

Geological environment

## Genesis This is a hydrothermal mineral, crystallizing in ore veins formed under moderate temperature conditions. It forms in polymetallic deposits rich in antimony, bismuth, silver, and lead. ## Mineral Associations At the type locality (Ánimas mine), it coexists with other sulfosalts, such as andorite, fizélyite, miargyrite, pyroxenite, as well as with pyrite, sphalerite, galena, and quartz. ## Localities The only confirmed and described occurrence of this mineral in the world is its type locality: the Colorada vein in the Ánimas mine, in the Chocaya-Animas mining district, Potosí Department, Bolivia.

Rarity

Extremely rare

For collectors

## Quality Criteria As an extremely rare mineral, any well-formed and analytically confirmed specimen is valuable. The most desirable samples are those with clearly visible, undamaged acicular crystals, preferably forming aesthetic aggregates on a rock matrix. Association with other rare sulfosalts is also important. ## Popular Localities The only source of specimens is the Ánimas mine in Bolivia, which is known for providing many rare and well-crystallized sulfosalts. Specimens from this locality are highly prized by collectors specializing in systematic mineralogy.

Care and storage

## Cleaning Specimens should only be cleaned mechanically, using a soft brush to remove dust. Due to its rarity and potential reactivity, contact with water and any chemical agents should be avoided. ## What to Avoid Avoid contact with chemicals, acids, and detergents, which can damage the mineral's surface. As a sulfosalt, it may be sensitive to moisture and oxidation in the long term. Protect it from high temperatures and sudden temperature changes. ## Storage It is recommended to store specimens in dry conditions, preferably in closed, padded collector boxes or display cases, to minimize the risk of mechanical damage and limit air exposure.

External references

Sources

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