Kostovite | |
---|---|
General | |
Category | Telluride mineral |
Formula (repeating unit) | AuCuTe4 |
IMA symbol | Ktv[1] |
Strunz classification | 2.EA.15 (10 ed) 2/D.16-10 (8 ed) |
Dana classification | 02.12.13.4 |
Crystal system | Orthorhombic |
Crystal class | Pyramidal (mm2) H-M Symbol: (mm2) |
Space group | Pma2 |
Identification | |
Color | Grayish white |
Twinning | Fine lamellar |
Cleavage | Distinct/good |
Tenacity | Brittle |
Mohs scale hardness | 2 – 2.5 |
Luster | Metallic |
Diaphaneity | Opaque |
Specific gravity | 7.94 |
Optical properties | Anisotropic |
Pleochroism | Visible |
References | [2][3][4][5][6] |
Kostovite (IMA symbol: Ktv) is a rare orthorhombic-pyramidal gray white telluride mineral containing copper and gold with chemical formula AuCuTe4.[2][3][4]
It was discovered by Bulgarian mineralogist Georgi Ivanov Terziev, who named it in honor of his professor Ivan Kostov (Иван Костов) (1913–2004).[7][8] In 1965 kostovite was approved as a new species by the International Mineralogical Association.[9] The type locality is Chelopech copper ore deposit, Bulgaria.[10] Small deposits have also been found in Kochbulak (Eastern Uzbekistan), Commoner mine (Zimbabwe), Kamchatka (Russian Far East), Ashanti (Ghana), Buckeye Gulch (Leadville, Colorado, US), Bisbee (Arizona, US),[11] Kutemajärvi (Finland), Coranda-Hondol (Romania), Glava (Sweden), Bereznjakovskoje (Southern Urals, Russia), Moctezuma (Sonora, Mexico), Panormos Bay (Tinos Island, Greece), Guilaizhuang Mine, Tongshi complex (Linyi Prefecture, Shandong Province, China), Kalgoorlie-Boulder City, (Goldfields-Esperance region, Western Australia, Australia).[12]