IRON ENRICHMENTS IN HYDROTHERMAL PLUMES OVER THE EAST PACIFIC RISE

dc.contributor.author	Hudson A.
dc.contributor.author	Bender M.L.
dc.contributor.author	Graham D.W.
dc.date.accessioned	2020-02-22T08:34:35Z
dc.date.available	2020-02-22T08:34:35Z
dc.date.issued	1986
dc.identifier	https://elibrary.ru/item.asp?id=31252005
dc.identifier.citation	EARTH AND PLANETARY SCIENCE LETTERS, 1986, 79, 3-4, 250-254
dc.identifier.issn	0012-821X
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/16002
dc.description.abstract	Manganese, iron, and helium isotopes have been measured in samples taken near the crest of the East Pacific Rise at 19°S. Samples were enriched in Mn and in He isotopes, as is typical for waters of this area. Samples were also enriched in Fe; Fe enrichments covary with Mn and3He enrichments. The Fe/Mn ratio at four sites ranged from about 2 to 9, spanning the average value found for metalliferous sediments (3.5).
dc.title	IRON ENRICHMENTS IN HYDROTHERMAL PLUMES OVER THE EAST PACIFIC RISE
dc.type	Статья

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