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dc.contributor.author | Sidorova E.U. | |
dc.contributor.author | Sitdikova L.M. | |
dc.contributor.author | Izotov V.G. | |
dc.contributor.author | Khasanova N.M. | |
dc.date.accessioned | 2021-02-25T06:52:56Z | |
dc.date.available | 2021-02-25T06:52:56Z | |
dc.date.issued | 2020 | |
dc.identifier.issn | 1755-1307 | |
dc.identifier.uri | https://dspace.kpfu.ru/xmlui/handle/net/161237 | |
dc.description.abstract | © 2020 IOP Publishing Ltd. All rights reserved. The studied weathering crust on the basement rocks of the central part of the Volga-Ural anteclise lies at great depths under thick sediments of sedimentary cover. A diversity of initial basement rocks, features of formation and secondary changing processes of weathering crust determine interest for this geological formation and its uniqueness. Clay minerals play a major role in the composition of the weathering crust and determine its features. A change in the associations of clay minerals by the weathering profile allows distinguishing different zones, which confirm the zonal structure of this formation. | |
dc.relation.ispartofseries | IOP Conference Series: Earth and Environmental Science | |
dc.title | The role of the leading formations of crystalline basement in the generation of clay minerals of weathering crust (East of the Russian plate) | |
dc.type | Conference Paper | |
dc.relation.ispartofseries-issue | 1 | |
dc.relation.ispartofseries-volume | 516 | |
dc.collection | Публикации сотрудников КФУ | |
dc.source.id | SCOPUS17551307-2020-516-1-SID85087447263 |