Important Update News
The RRUFF Project has been migrated to RRUFF.net. Please update your bookmarks immediately, if you have not done so.
The data on this website is already three years out of date, and the entire website will be taken offline before the end of the year.
We are grateful to NASA for the funding of this effort.
|
|
Name: Teallite RRUFF ID: R060487 Ideal Chemistry: PbSnS2 Locality: Porvenir mine, Huanuni, Department of Oruro, Bolivia Source: Michael Scott S100329 [view label] Owner: RRUFF Description: Grayish black platy metallic mass Status: The identification of this mineral has been confirmed by X-ray diffraction and chemical analysis |
| Mineral Group: [ Arsenolamprite (3) ] | ||
| Quick search: [ All Teallite samples (2) ] | ||
| CHEMISTRY | ||||||||
|---|---|---|---|---|---|---|---|---|
|
|
|||||||
| RAMAN SPECTRUM | ||||||||||||
|---|---|---|---|---|---|---|---|---|---|---|---|---|
|
||||||||||||
| BROAD SCAN WITH SPECTRAL ARTIFACTS | ||||||||||||
|---|---|---|---|---|---|---|---|---|---|---|---|---|
|
||||||||||||
| POWDER DIFFRACTION | ||||||||
|---|---|---|---|---|---|---|---|---|
| RRUFF ID: | R060487.1 | |||||||
| Sample Description: | Powder | |||||||
| Cell Refinement Output: |
a: 11.335(3)Å b: 4.040(2)Å c: 4.2871(9)Å alpha: 90.° beta: 90.° gamma: 90.° Volume: 196.35(9)Å3 Crystal System: orthorhombic |
|||||||
|
|
|||||||
| REFERENCES for Teallite | |
|---|---|
|
American Mineralogist Crystal Structure Database Record: [view record] |
|
|
Anthony J W, Bideaux R A, Bladh K W, and Nichols M C (1990) Handbook of Mineralogy, Mineral Data Publishing, Tucson Arizona, USA, by permission of the Mineralogical Society of America. [view file] |
|
|
Prior G T (1904) On teallite, a new sulphostannite of lead from Bolivia; and its relations to frankeite and cylindrite, Mineralogical Magazine, 14, 21-27 [view file] |
|
|
Sejkora J, Berlepsch P, Makovicky E, Balić-unić T, Litochleb J (2002) Teallite from Radvanice near Trutnov (Czech Republic), Neues Jahrbuch für Mineralogie, Abhandlungen, 177, 163-180 |
|
|
|