Pearcbuteite | |
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General | |
Category | Mineral |
Formula (repeating unit) | Cu(Ag,Cu)6Ag9As2S11[1] |
IMA symbol | Pea[2] |
Strunz classification | 2.GB.15 (10 ed) 2/E.05-20 (8 ed) |
Dana classification | 3.1.8.1 |
Crystal system | Monoclinic or trigonal |
Space group | P3m1 (no. 164) |
Identification | |
Formula mass | 2,096.80 g/mol |
Color | Black |
Crystal habit | Pseudohexagonal prisms |
Cleavage | {001} Poor[3] |
Fracture | Conchoidal to irregular |
Tenacity | Brittle |
Mohs scale hardness | 3 |
Luster | Metallic |
Streak | Black |
Diaphaneity | Opaque |
Specific gravity | 6.15 |
Optical properties | Biaxial |
Refractive index | 2.7 |
Birefringence | 2.7 |
Pleochroism | RL Pleochroism (in reflected plane polarised light): Very weak in air, fair in oil[3][4] |
Other characteristics | Non-fluorescent, nonmagnetic, not radioactive |
References | [3][4][5][6] |
Pearceite is one of the four so-called "ruby silvers", pearceite Cu(Ag,Cu)6Ag9As2S11, pyrargyrite Ag3SbS3, proustite Ag3AsS3 and miargyrite AgSbS2.[6] It was discovered in 1896 and named after Dr Richard Pearce (1837–1927), a Cornish–American chemist and metallurgist from Denver, Colorado.[4]