Fettelite, also known as sanguinite, is a mercury-
sulfosalt mineral with the chemical formula Ag
16HgAs
4S
15. 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
The Odenwald () is a low mountain range in the Germany, German states of Hesse, Bavaria and Baden-Württemberg.
Location
The Odenwald is located between the Upper Rhine Plain with the Bergstraße Route, Bergstraße and the ''Hessisches Ried' ...
.
It was first collected in the Nieder-Beerbach mine, 10 km south of
Darmstadt
Darmstadt () is a city in the States of Germany, state of Hesse in Germany, located in the southern part of the Frankfurt Rhine Main Area, Rhine-Main-Area (Frankfurt Metropolitan Region). Darmstadt has around 160,000 inhabitants, making it the ...
,
Odenwald
The Odenwald () is a low mountain range in the Germany, German states of Hesse, Bavaria and Baden-Württemberg.
Location
The Odenwald is located between the Upper Rhine Plain with the Bergstraße Route, Bergstraße and the ''Hessisches Ried' ...
,
Germany
Germany, officially the Federal Republic of Germany, is a country in Central Europe. It lies between the Baltic Sea and the North Sea to the north and the Alps to the south. Its sixteen States of Germany, constituent states have a total popu ...
. Its normal occurrence is in
hydrothermal veins, which can cut
gabbro
Gabbro ( ) is a phaneritic (coarse-grained and magnesium- and iron-rich), mafic intrusive igneous rock formed from the slow cooling magma into a holocrystalline mass deep beneath the Earth's surface. Slow-cooling, coarse-grained gabbro is ch ...
-
diorite
Diorite ( ) is an intrusive rock, intrusive igneous rock formed by the slow cooling underground of magma (molten rock) that has a moderate content of silica and a relatively low content of alkali metals. It is Intermediate composition, inter ...
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 sub parallel aggregates can be measured.][ Mandarino, J.A (1997) Abstracts of new mineral description The Mineralogical Record, 28, 141-143. ] The birefringence of Fettelite is moderate white to grayish brown.[
]
References
Arsenic minerals
Mercury(II) minerals
Silver minerals
Sulfosalt minerals
Monoclinic minerals
Minerals in space group 5
Minerals described in 1996
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