ISOTOPIC COMPOSITION OF THE SULFUR IN PYRITE AND PYRRHOTITE SYNTHESIZED AT 300 TO 500°C AND 1 KBAR
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dc.contributor.author | Likhoydov G.G. | |
dc.contributor.author | Suvorova V.A. | |
dc.date.accessioned | 2020-10-11T11:11:57Z | |
dc.date.available | 2020-10-11T11:11:57Z | |
dc.date.issued | 1989 | |
dc.identifier | https://elibrary.ru/item.asp?id=31165802 | |
dc.identifier.citation | Transactions (Doklady) of the USSR Academy of Sciences. Earth Science Sections, 1989, , 4, 221-224 | |
dc.identifier.issn | 0891-5571 | |
dc.identifier.uri | https://repository.geologyscience.ru/handle/123456789/17964 | |
dc.description.abstract | The isotopic composition of the sulfur in synthetic pyrite (Pt) and pyrrhotite (Pr) was studied as a function of the reaction temperature (T) and oxygen fugacity fO2. These minerals were synthesized by the hydrothermal process in ampoules placed in an autoclave. The pressure Ptot was 1 kbar, and the temperatures were 300°, 400° and 500°C. The pressure was controlled by the degree of filling of the autoclave. The temperature was measured with an error of ±10°C. Preliminary experiments on kinetics of the reaction proved that the reactions go to completion in 30 to 40 hours. No changes were discernible by our analytical method after that time. | |
dc.title | ISOTOPIC COMPOSITION OF THE SULFUR IN PYRITE AND PYRRHOTITE SYNTHESIZED AT 300 TO 500°C AND 1 KBAR | |
dc.type | Статья |
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