Nickel-free iron particles in sediments

dc.contributor.author	Pechersky D.
dc.contributor.author	Kuzina D.
dc.date.accessioned	2018-09-18T20:18:13Z
dc.date.available	2018-09-18T20:18:13Z
dc.date.issued	2015
dc.identifier.issn	1069-3513
dc.identifier.uri	https://dspace.kpfu.ru/xmlui/handle/net/138500
dc.description.abstract	© 2015, Pleiades Publishing, Ltd. The results provided by the microprobe and thermomagnetic studies of native iron in sediments are generalized. It is found that the sediments are abundant in Ni-free iron particles. These particles are shown to have extraterrestrial origin and likely to be parts of cosmic dust. It is suggested that these particles were formed from the mantle and crustal rocks as a result of their fragmentation and melting of the silicates (such as olivine and pyroxene) contained in these rocks.
dc.relation.ispartofseries	Izvestiya, Physics of the Solid Earth
dc.title	Nickel-free iron particles in sediments
dc.type	Article
dc.relation.ispartofseries-issue	6
dc.relation.ispartofseries-volume	51
dc.collection	Публикации сотрудников КФУ
dc.relation.startpage	897
dc.source.id	SCOPUS10693513-2015-51-6-SID84942441401

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Публикации сотрудников КФУ Scopus [24551]
Коллекция содержит публикации сотрудников Казанского федерального (до 2010 года Казанского государственного) университета, проиндексированные в БД Scopus, начиная с 1970г.