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Cosmic microspheres in the Carboniferous deposits of the Usolka section (Urals foredeep)

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dc.contributor.author Sungatullin R.
dc.contributor.author Sungatullina G.
dc.contributor.author Zakirov M.
dc.contributor.author Tsel'movich V.
dc.contributor.author Glukhov M.
dc.contributor.author Bakhtin A.
dc.contributor.author Osin Y.
dc.contributor.author Vorob'ev V.
dc.date.accessioned 2018-09-19T20:58:17Z
dc.date.available 2018-09-19T20:58:17Z
dc.date.issued 2017
dc.identifier.issn 1068-7971
dc.identifier.uri https://dspace.kpfu.ru/xmlui/handle/net/143472
dc.description.abstract © 2017Magnetite microspheres from the Carboniferous deposits of the Usolka reference section were studied by probe microanalysis, with comparison of the distributions of chemical elements and microspheres. The presence of microspheres in sedimentary strata is considered to be an additional factor for stratigraphic correlation between sedimentary sections. The microspheres are shown to be of cosmic nature. The Late Paleozoic paleoclimatic changes (extreme cooling) and biotic crises were caused by the periodical Solar System motion in the Galaxy, cosmic-dust fallout, and meteorite bombardments of the Earth.
dc.relation.ispartofseries Russian Geology and Geophysics
dc.subject Carboniferous
dc.subject chemical composition
dc.subject cosmic bombardment
dc.subject magnetite microspheres
dc.subject paleoclimate
dc.subject Urals foredeep
dc.title Cosmic microspheres in the Carboniferous deposits of the Usolka section (Urals foredeep)
dc.type Article
dc.relation.ispartofseries-issue 1
dc.relation.ispartofseries-volume 58
dc.collection Публикации сотрудников КФУ
dc.relation.startpage 59
dc.source.id SCOPUS10687971-2017-58-1-SID85013170790


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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.

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