Dyscrasite
In today's world, Dyscrasite is still a topic of great relevance and debate. Whether due to its impact on society, its influence on popular culture or its importance in everyday life, Dyscrasite continues to be a topic of interest for people of all ages and backgrounds. From its origins to its evolution today, Dyscrasite has been the subject of numerous studies, analyzes and discussions that seek to better understand its scope and meaning. In this article, we will explore different aspects of Dyscrasite and examine its importance in the current context.
| Dyscrasite | |
|---|---|
 Twinned dyscrasite crystals from the Czech Republic (size: 4.5 × 4.5 × 3.3 cm) | |
| General | |
| Category | Antimonide minerals |
| Formula | Ag3+xSb1−x (x ≈ 0.2) |
| IMA symbol | Dys[1] |
| Strunz classification | 2.AA.35 |
| Crystal system | Orthorhombic |
| Crystal class | Pyramidal (mm2) H-M symbol: (mm2) |
| Space group | Pmm2 |
| Unit cell | a = 3.008, b = 4.828 c = 5.214 ; Z = 1 |
| Identification | |
| Color | Silver-white (tarnishes to lead-gray, yellowish, or black) |
| Crystal habit | Pyramidal crystals also cylindrical, prismatic to platy, striated; granular, foliated or massive |
| Twinning | On {110} produces pseudohexagonal forms |
| Cleavage | Distinct on {001} {001}, imperfect on {110} |
| Fracture | Irregular or uneven |
| Tenacity | Sectile |
| Mohs scale hardness | 3+1⁄2 – 4 |
| Luster | Metallic |
| Streak | Silver-white |
| Diaphaneity | Opaque |
| Specific gravity | 9.4 – 10 |
| Birefringence | Very weak |
| Pleochroism | Very weak |
| Other characteristics | Weakly anisotropic |
| References | [2][3][4] |
The silver antimonide mineral dyscrasite has the chemical formula Ag3Sb. It is an opaque, silver white, metallic mineral which crystallizes in the orthorhombic crystal system. It forms pyramidal crystals up to 5 cm (2.0 in) and can also form cylindrical and prismatic crystals.[2]
Crystallography and properties
Dyscrasite is a metal ore and is opaque. In reflected light, however, it demonstrates weak anisotropism. Dyscrasite’s color under plane polarized light is most likely dark grey/black. When spun on a rotatable stage of a microscope (under plane polarized light), dyscrasite’s color should slightly change shades. This property is called pleochroism. Dyscrasite exhibits very weak reflected light pleochroism.[4]
Dyscrasite belongs to the orthorhombic crystal class, meaning all three of its axes (a, b, and c) are unequal in length and are 90° to each other.[5]
Discovery and occurrence
It was first described for an occurrence in 1797 in the Wenzel Mine, Black Forest, Germany. The name dyscrasite comes from the Greek word δυσκράσις, meaning "a bad alloy."[3]
It occurs as a hydrothermal mineral in silver bearing veins in association with native silver, pyrargyrite, acanthite, stromeyerite, tetrahedrite, allemontite, galena, calcite and baryte.[2]
See also
References
- ^ Warr, L.N. (2021). "IMA–CNMNC approved mineral symbols". Mineralogical Magazine. 85 (3): 291–320. Bibcode:2021MinM...85..291W. doi:10.1180/mgm.2021.43. S2CID 235729616.
- ^ a b c Anthony, J.W., Bideau, R.A., Bladh, K.W., and Nichols, M.C. (1990) Handbook of Mineralogy: Volume I: Elements, Sulfides, Sulfosalts. 588 p. Mineral Data Publishing, Tucson, Arizona. http://rruff.geo.arizona.edu/doclib/hom/dyscrasite.pdf
- ^ a b Mindat.org
- ^ a b Webmineral data
- ^ Klein, C., and Dutrow, B. (2007) The Manual of Mineral Science, 23rd ed. 675 p. John Wiley & Sons, Inc. Hoboken, New Jersey.
