| Reference Type | Journal (article/letter/editorial) |
|---|
| Access Rights | Open Access |
|---|
| Title | Wittichenite, Cu3BiS3, from Tokke and Fyresdal in west Telemark. Contributions to the mineralogy of Norway, no. 49 |
|---|
| Journal | Norsk Geologisk Tidsskrift
[Norwegian Journal of Geology] | ISSN | 0029-196X |
|---|
| Authors | Nordrum, Fred Steinar | Author |
|---|
| Year | 1972 | Volume | 52 |
|---|
| Page(s) | 257-271 | Issue | 3 |
|---|
| Publisher | Norsk Geologisk Forening (Geological Society of Norway) |
|---|
| URL | |
|---|
| Download URL | https://njg.geologi.no/images/NJG_articles/NGT_52_3_257-271.pdf+ |
|---|
| Classification | Not set | LoC | Not set |
|---|
| Mindat Ref. ID | 16616800 | Long-form Identifier | mindat:1:5:16616800:6 |
|---|
|
| GUID | 18513a74-8265-4ae7-a440-f407e94f7d27 |
|---|
| Full Reference | Nordrum, Fred Steinar (1972) Wittichenite, Cu3BiS3, from Tokke and Fyresdal in west Telemark. Contributions to the mineralogy of Norway, no. 49. Norsk Geologisk Tidsskrift [Norwegian Journal of Geology], 52 (3) Norsk Geologisk Forening (Geological Society of Norway) 257-271 |
|---|
| Plain Text | Nordrum, Fred Steinar (1972) Wittichenite, Cu3BiS3, from Tokke and Fyresdal in west Telemark. Contributions to the mineralogy of Norway, no. 49. Norsk Geologisk Tidsskrift [Norwegian Journal of Geology], 52 (3) Norsk Geologisk Forening (Geological Society of Norway) 257-271 |
|---|
| In | (1972) Norsk Geologisk Tidsskrift [Norwegian Journal of Geology] Vol. 52 (3) Norsk Geologisk Forening (Geological Society of Norway) |
|---|
| Abstract/Notes | The first occurrence of wittichenite, Cu3BiS3, in Norway is reported from hydrothermal quartz veins in west Telemark. X-ray and optical data are given and are compared with the data for wittichenite reported so far. A variety of intergrowth textures of wittichenite with bornite, chalcopyrite, chalcocite, and galena is described. The characteristic development of a secondary mineral - 'X' - is useful for identification of wittichenite in ores occurring near the surface. Wittichenite and the associated chalcopyrite were formed as replacement products, when bismuth from Bi, Pb-bearing hydrothermal solutions reacted with bornite |
|---|
These are possibly similar items as determined by title/reference text matching only.
