| Reference Type | Journal (article/letter/editorial) |
|---|
| Title | Mackinawite, pentlandite, and native copper from the Newport pallasite |
|---|
| Journal | Mineralogical Magazine and Journal of the Mineralogical Society |
|---|
| Authors | Buseck, Peter R. | Author |
|---|
| Year | 1968 (March) | Volume | 36 |
|---|
| Issue | 281 |
|---|
| Publisher | Mineralogical Society |
|---|
| Download URL | https://rruff.info/doclib/MinMag/Volume_36/36-281-717.pdf+ |
|---|
| DOI | doi:10.1180/minmag.1968.036.281.13Search in ResearchGate |
|---|
| Generate Citation Formats |
|---|
| Mindat Ref. ID | 6141 | Long-form Identifier | mindat:1:5:6141:8 |
|---|
|
| GUID | 0 |
|---|
| Full Reference | Buseck, Peter R. (1968) Mackinawite, pentlandite, and native copper from the Newport pallasite. Mineralogical Magazine and Journal of the Mineralogical Society, 36 (281) 717-725 doi:10.1180/minmag.1968.036.281.13 |
|---|
| Plain Text | Buseck, Peter R. (1968) Mackinawite, pentlandite, and native copper from the Newport pallasite. Mineralogical Magazine and Journal of the Mineralogical Society, 36 (281) 717-725 doi:10.1180/minmag.1968.036.281.13 |
|---|
| In | (1966) Mineralogical Magazine Vol. 36 (281) Mineralogical Society |
|---|
| Abstract/Notes | SummaryThese minerals indicate strongly reducing conditions as well as extremely low sulphur fugacities within the Newport pallasite. They all formed at low temperatures (upper limit 580° C) and in the solid state. This is the first reported occurrence of mackinawite and pentlandite from a pallasitic meteorite; Cu is known from only one other pallasite. Microprobe analyses of a large Cu grain indicate its composition as 98·6 ± 0·5 %, Ni 2·0 ± 0·5, Fe below the limit of detection (∼0.3). |
|---|
These are possibly similar items as determined by title/reference text matching only.
