THE ZERKALY CHONDRITIC METEORITE

dc.contributor.author	Agafonov L.V.
dc.contributor.author	Kuznetsov S.M.
dc.contributor.author	Pospelova L.N.
dc.date.accessioned	2022-07-20T06:12:23Z
dc.date.available	2022-07-20T06:12:23Z
dc.date.issued	2004
dc.identifier	https://www.elibrary.ru/item.asp?id=13459921
dc.identifier.citation	Doklady Earth Sciences, 2004, 396, 4, 515-518
dc.identifier.issn	1028-334X
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/38332
dc.description.abstract	The Zerkaly chondritic meteorite belongs to the high-Fe (olivine-bronzite) type H5, with a severely limonitized matrix. Like chondrules, the matrix is characterized by nonuniform texture. The meteorite underwent secondary heating and deformation on the Earth, probably resulting in deterioration of its primary textures, structures, mineral composition, and even chemical composition to a variable extent.
dc.title	THE ZERKALY CHONDRITIC METEORITE
dc.type	Статья

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