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The Major Types of the Weathering Crust of the Eastern Russian Plate and its Mineralogical and Geochemical Features

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dc.contributor Казанский федеральный университет
dc.contributor.author Izotov Viktor Gennadevich
dc.contributor.author Sidorova Elena Urevna
dc.contributor.author Sitdikova Lyalya Mirsalichovna
dc.date.accessioned 2016-01-29T11:23:32Z
dc.date.available 2016-01-29T11:23:32Z
dc.date.issued 2015
dc.identifier.citation Sidorova Elena, Sitdikova Lyalya, Izotov Victor. The Major Types of the Weathering Crust of the Eastern Russian Plate and its Mineralogical and Geochemical Features // Procedia Earth and Planetary Science. - 2015. - Vol. 15. - PP. 573-578.
dc.identifier.issn
dc.identifier.uri http://dspace.kpfu.ru/xmlui/handle/net/32811
dc.description.abstract The long continental period in the East of the Russian plate (the upper Proterozoic ? the middle Devonian) caused the formation of a weathering crust on the crystalline basement rocks. In pre-Devonian time, due to the washing-out and the subsequent processes of redeposition of substance, two types of weathering crust were formed: displaced and non-displaced. The widespread weathering crust of the crystalline basement of the East of the Russian plate is a unique object for studying the mineral formation processes of ancient weathering. Complex mineralogical and geochemical studies of the weathering crust are of practical value for the creation of a full picture of the development of the deep horizons of the earth crust and a forecast of mineral deposits.
dc.language.iso en
dc.relation.ispartofseries Procedia Earth and Planetary Science
dc.rights открытый доступ
dc.subject Weathering crust
dc.subject crystalline basement
dc.subject Tatar arch
dc.title The Major Types of the Weathering Crust of the Eastern Russian Plate and its Mineralogical and Geochemical Features
dc.type Article
dc.contributor.org Институт геологии и нефтегазовых технологий
dc.description.pages
dc.pub-id 112906


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