THE SYSTEM FE-PT-S AT 1100°C
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| dc.contributor.author | Majzlan J. | |
| dc.contributor.author | Makovicky M. | |
| dc.contributor.author | Makovicky E. | |
| dc.contributor.author | Rose-Hansen J. | |
| dc.date.accessioned | 2021-06-11T04:57:57Z | |
| dc.date.available | 2021-06-11T04:57:57Z | |
| dc.date.issued | 2002 | |
| dc.identifier | https://elibrary.ru/item.asp?id=13685836 | |
| dc.identifier.citation | The Canadian Mineralogist, 2002, 40, 2, 509-517 | |
| dc.identifier.issn | 0008-4476 | |
| dc.identifier.uri | https://repository.geologyscience.ru/handle/123456789/29037 | |
| dc.description.abstract | The system Fe–Pt–S at 1100°C contains four alloys, γ(Fe,Pt), PtFe, Pt3Fe and γ (Pt, Fe), with respective miscibility-gaps at 43.5–45.5 at.% Pt, 57.7–60.4 at.% Pt and 77–80 at.% Pt, two sulfide phases, Fe1− x S (maximum Pt solubility 1.1 at.% at 54.3 at.% S) and PtS (0.5–0.8 at.% Fe maximum), a Fe-rich sulfide melt (Pt solubility below microprobe limits) and a S-rich sulfide melt (Pt solubility 7.5 at.% for solidified melts with ~54.5 at.% S). Of the five two-phase and five three-phase associations, the most important are PtFe – Pt3Fe – Fe1− x S (Pt below detection), Pt3Fe – Fe1− x S (0.4 at.% Pt) – PtS, Pt3Fe – γ (Pt,Fe) – PtS and Fe1− x S (0.9 at.% Pt) – melt (~8.5 at.% Pt) – PtS. Comparisons of experimental data with natural associations enable us to suggest several genetic and geothermometric implications. | |
| dc.subject | system Fe–Pt–S | |
| dc.subject | iron–platinum alloys | |
| dc.subject | isoferroplatinum | |
| dc.subject | monosulfide solid-solution | |
| dc.subject | cooperite | |
| dc.title | THE SYSTEM FE-PT-S AT 1100°C | |
| dc.type | Статья |
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