Bilibinskite: Difference between revisions
refined link |
correction |
||
| Line 44: | Line 44: | ||
Bilibinskite is a [[metal]]lic [[mineral]] with a color that ranges from opaque bronze-colored to light-brown or brownish-pink. It has a sub-metallic luster, a brown stripe color and has no fission. Bilibinskite crystallizes in the [[Cubic crystal system|cubic system]]. It has a high relative [[density]] of 14.27. The mineral has a [[hardness]] of 4.5 to 5 and it is not radioactive. |
Bilibinskite is a [[metal]]lic [[mineral]] with a color that ranges from opaque bronze-colored to light-brown or brownish-pink. It has a sub-metallic luster, a brown stripe color and has no fission. Bilibinskite crystallizes in the [[Cubic crystal system|cubic system]]. It has a high relative [[density]] of 14.27. The mineral has a [[hardness]] of 4.5 to 5 and it is not radioactive. |
||
==Occurrence== |
==Occurrence== |
||
Bilibinskite is a very rare mineral that formed in the weathering zones of [[gold telluride]]s. The [[Type locality (geology)|type locality]] is the [[Kamchatka Peninsula]] in the [[Russian Far East]], where the mineral was discovered in 1978. It has |
Bilibinskite is a very rare mineral that formed in the weathering zones of [[gold telluride]]s. The [[Type locality (geology)|type locality]] is the [[Kamchatka Peninsula]] in the [[Russian Far East]], where the mineral was discovered in 1978. It has also been found n [[hypogene]] ores of [[Kazakhstan]], [[Xinjiang]] and [[Tuva]].<ref>I.Y. Nekrasov, ''Geochemistry, Mineralogy and Genesis of Gold Deposits'', table 20.</ref> |
||
==See also== |
==See also== |
||
Revision as of 08:00, 20 November 2019
| Bilibinskite | |
|---|---|
| General | |
| Category | Telluride mineral |
| Formula (repeating unit) | Au3Cu2PbTe2 |
| Strunz classification | 02.BA.55 |
| Crystal system | Cubic |
| Crystal class | Sulfide |
| Identification | |
| Formula mass | 1,180.39 g/mol |
| Color | Bronze colored, light brown or brownish-pink |
| Crystal habit | Massive |
| Cleavage | None |
| Mohs scale hardness | 4.5 - 5 |
| Luster | Sub-metallic |
| Streak | golden brown |
| Diaphaneity | opaque |
| Density | 14.27 |
| Optical properties | Anisotropic |
| Other characteristics | IMA Status Approved (1978) |
| References | [1][2] |
Bilibinskite is a Au - Cu - Pb telluride. It is is a rare mineral that was named after Soviet geologist Yuri Bilibin (1901–1952), who researched the geology of gold deposits during the time of the USSR.
Properties
Bilibinskite is a metallic mineral with a color that ranges from opaque bronze-colored to light-brown or brownish-pink. It has a sub-metallic luster, a brown stripe color and has no fission. Bilibinskite crystallizes in the cubic system. It has a high relative density of 14.27. The mineral has a hardness of 4.5 to 5 and it is not radioactive.
Occurrence
Bilibinskite is a very rare mineral that formed in the weathering zones of gold tellurides. The type locality is the Kamchatka Peninsula in the Russian Far East, where the mineral was discovered in 1978. It has also been found n hypogene ores of Kazakhstan, Xinjiang and Tuva.[3]
See also
References
- ^ Bilibinskite - Russian Foundation for Basic Researches
- ^ Handbook of Mineralogy
- ^ I.Y. Nekrasov, Geochemistry, Mineralogy and Genesis of Gold Deposits, table 20.