Показать сокращенную информацию
dc.contributor.author | Bulka G. | |
dc.contributor.author | Nizamutdinov N. | |
dc.contributor.author | Mukhutdinova N. | |
dc.contributor.author | Khasanova N. | |
dc.contributor.author | Galeev A. | |
dc.contributor.author | Vinokurov V. | |
dc.date.accessioned | 2018-09-17T20:53:27Z | |
dc.date.available | 2018-09-17T20:53:27Z | |
dc.date.issued | 1991 | |
dc.identifier.issn | 0937-9347 | |
dc.identifier.uri | https://dspace.kpfu.ru/xmlui/handle/net/134210 | |
dc.description.abstract | EPR data (i.e. the distribution of Mn2+ in carbonate rocks and of free radicals in terrigenous rocks) may be used to characterize sedimentary beds, especially if they are unfossilferous. The study of the distribution of Mn2+ that substitutes Mg2+ and Ca2+ in sedimentary dolomites suggests that the distribution is affected by their genesis. © 1991 Springer. | |
dc.relation.ispartofseries | Applied Magnetic Resonance | |
dc.title | EPR probes in sedimentary rocks: The features of Mn2- and free radicals distribution in the Permian formation in Tatarstan | |
dc.type | Article | |
dc.relation.ispartofseries-issue | 1 | |
dc.relation.ispartofseries-volume | 2 | |
dc.collection | Публикации сотрудников КФУ | |
dc.relation.startpage | 107 | |
dc.source.id | SCOPUS09379347-1991-2-1-SID69449091507 |