ISOTOPIC COMPOSITION OF THE SULFUR IN PYRITE AND PYRRHOTITE SYNTHESIZED AT 300 TO 500°C AND 1 KBAR

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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