Markwelchite

markwelchite

guettardite

twinnite

protochabourneite

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Formula: TlPbSbS3
Sulphosalt, thallium- and antimony- bearing mineral
Crystal System: Monoclinic
Specific gravity: 6.696 calculated for the empirical formula
Hardness: 3 to 4
Streak: Black
Colour: Black
Environments


Hydrothermal environments

Markwelchite is a new mineral, approved in 2024 and to date (October 2024) reported only from the type locality.

Localities

At the type locality, Jas Roux, La Chapelle-en-Valgaudemar, Gap, Hautes-Alpes, Provence-Alpes-Côte d'Azur, France, the deposit is hosted in dolomitic metalimestones of Triassic age (251.902 to 201.4 million years ago) and appears as several sedimentary lenses embedded in anatexites. These lenses protrude and form small cliffs parallel to the valley. Samples studied consist of boulders weathered out of the cliffs which contained small veinlets of primary sulphosalts accompanied by a variety of secondary minerals.
Markwelchite is associated with stibnite, twinnite, guettardite, pierrotite, realgar and protochabournéite. The formation of markwelchite is linked to the activity of thallium - lead - antimony rich fluids during the hydrothermal evolution of the Jas Roux deposit. The markwelchite occurs as black anhedral crystals up to 40 μm in size; it is opaque with a metallic lustre and a black streak (MM 88.503–509).

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