PLAGIONITE
Class : Sulfides and sulfosalts
Subclass : Sulfosalts
Crystal system : Monoclinic
Chemistry : Pb5Sb8S17
Rarity : Rare to very rare
Plagionite is a rare sulfosalt of medium-temperature lead-antimony hydrothermal veins. It is found just like boulangerite, semseyite, zinkenite or jamesonite in dominantly stibnite veins invaded by lead-bearing fluids, or in galena-sphalerite veins infiltrated by antimony fluids. It commonly accompanies stibnite, bournonite and other sulfosalts of lead and antimony; however, it is clearly rarer than the latter. Its name comes from the Greek plagios (oblique) in allusion to its monoclinic crystals. Plagionite occurs in tabular crystals up to 1 cm thick, flattened according to {001}, sometimes in short prisms, and commonly remains massive, grainy to compact. The color is lead gray, the luster is metallic. Plagionite alters easily in outcrops giving mixtures of antimony oxides and various lead oxides.
Main photo : Plagionite from Graf Jost-Christian Mine, Wolfsberg, Germany © Uwe Haubenreisser
Plagionite in the World
Twinning
No twin known for this mineral species.
Fakes and treatments
No fakes listed for this mineral species.
Hardness : 2.5
Density : 5.54 to 5.58
Fracture : Irregular to conchoidal
Streak : Grey-black to red-brown
TP : Opaque
RI : -
Birefringence : -
Optical character : -
Pleochroism : None
Fluorescence : None
Solubility : Hydrochloric acid
Magnetism : NoneRadioactivity : None