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 |
|