Fettelite, also known as sanguinite, is a mercury-sulfosalt mineral with the chemical formula Ag16HgAs4S15. It is a rare Silver Mercury Arsenic Sulfosalt forming silvery to blood red platy micro-crystals. The specimen is almost certainly from the Glasberg Quarry, Nieder-Beerbach, Germany. It is a monoclinic-sphenoidal grayish white mineral containing antimony, arsenic, copper, iron, lead, mercury, silver, sulfur, and thallium.
The mineral was first described by Wang and Paniagua (1996) who named it after M. Fettel, a German field geologist who collected the first samples from Odenwald. It was first collected in the Nieder-Beerbach mine, 10 km south of Darmstadt, Odenwald, Germany.
- Category: Sulfosalt mineral
- Formula: Ag16HgAs4S15
- Crystal system: Monoclinic
- Crystal class: Sphenoidal (2) (same H-M symbol)
Fig: Fettelite, also known as sanguinite
The specimen of this rare mineral we have has abundant crystals of Fettelite with colorless crystals of Calcite. In rare associated with ‘Proustite’ and other undefined silver species.
- Color: dark violet to red
- Crystal habit: flakes, hexagonal, micaceous
- Cleavage: perfect
- Fracture: subconchoidal
- Mohs scale hardness: 3.5
- Luster: metallic
- Streak: dark vermillion
- Diaphaneity: subopaque to opaque
- Specific gravity: 6.29
- Optical properties: Biaxial, anisotrophism weak with strong red internal reflections
Its normal occurrence is in hydrothermal veins, which can cut gabbro-diorite intrusives. It is closely related to other rare minerals like dervillite, daomanite, vaughanite and criddleite which are also found in the same type locality as fettelite.
Fettelite occurs as clusters of hexagonal flakes. These flakes can get up to 0.2 mm across and around 5-10 µm thick. In more complex hexagonal tablets, somewhat larger subparallel aggregates can be measured. The birefringence of Fettelite is moderate white to grayish brown.