UM1989-28-Se:AgBiCuS
Valid as an unnamed mineral
This page is currently not sponsored. Click here to sponsor this page.
Formula:
(Ag,Cu)Bi3(Se,S)5
Unique combination of elements. Co-described with 'UM1989-27-Se:AgAsFeS' and 'UM1989-29-Se:Te'.
Probably a Cu-bearing variety of Unnamed (Se-analogue of Pavonite).
Occurs as grains, 60-80 microns in size, occurring close to gold and a phase corresponding to (Bi,As,Te,Se)2O3, all within quartz.
Likely formed due to fSe activity increase at ca. 150-200oC; relatively late-stage species.
Probably a Cu-bearing variety of Unnamed (Se-analogue of Pavonite).
Occurs as grains, 60-80 microns in size, occurring close to gold and a phase corresponding to (Bi,As,Te,Se)2O3, all within quartz.
Likely formed due to fSe activity increase at ca. 150-200oC; relatively late-stage species.
Unique Identifiers
Mindat ID:
51681
Long-form identifier:
mindat:1:1:51681:7
GUID
(UUID V4):
(UUID V4):
f3bea066-6e05-4589-ae50-cd6d412c0920
Classification of UM1989-28-Se:AgBiCuS
IMA status notes:
Unnamed (probably valid)
Optical Data of UM1989-28-Se:AgBiCuS
Anisotropism:
strong
Bireflectance:
weak
Colour in reflected light:
light gray with a bluish tint
Chemical Properties of UM1989-28-Se:AgBiCuS
Formula:
(Ag,Cu)Bi3(Se,S)5
Other Information
Health Risks:
No information on health risks for this material has been entered into the database. You should always treat mineral specimens with care.
References for UM1989-28-Se:AgBiCuS
Reference List:
Localities for UM1989-28-Se:AgBiCuS
Locality List
- This locality has map coordinates listed.
- This locality has estimated coordinates.
ⓘ - Click for references and further information on this occurrence.
? - Indicates mineral may be doubtful at this locality.
- Good crystals or important locality for species.
- World class for species or very significant.
(TL) - Type Locality for a valid mineral species.
(FRL) - First Recorded Locality for everything else (eg varieties).
Struck out - Mineral was erroneously reported from this locality.
Faded * - Never found at this locality but inferred to have existed at some point in the past (e.g. from pseudomorphs).
All localities listed without proper references should be considered as questionable.
All localities listed without proper references should be considered as questionable.
Russia | |
| Kovalenker, V.A. , Nekrasov, L.Ya., Sandomirskaya, S.M., Nekrasova, A.N., Malov, V.S., Danchenko, V.Ya., Dmitriyeva, M.T.(1989)" Sulfide-selenide-telluride mineralization of epithermal manifestations of the Kurile-Kamchatka volcanic belt. Mineral. Zhurnal: 11(6): 3-18 (in Russian); in: Jambor, J.L., Grew, E.S. (1992): New mineral Names. American Mineralogist: 77: 210 |