Form of presentation | Conference proceedings in Russian journals and collections |
Year of publication | 2014 |
Язык | русский |
|
Linkina Larisa Igorevna, author
Petrova Elena Vitalevna, author
|
Bibliographic description in the original language |
E. Petrova, L. Linkina To the Question of boundaries and composition of Gelasian Stratum in the Middle Volga Region / THE QUATERNARY OF THE URALS: global trends and Pan-European Quaternary records Ekaterinburg, Russia September 10–16, 2014 Ekaterinburg UrFU 2014 International conference INQUA-SEQS 2014. R. 113-115.
|
Annotation |
THE QUATERNARY OF THE URALS: global trends and Pan-European Quaternary records |
Keywords |
quaternary system, Gelasian Stratum, Akchagyl regio-stage,Middle Volga Region. |
The name of the journal |
THE QUATERNARY OF THE URALS: global trends and Pan-European Quaternary records
|
Please use this ID to quote from or refer to the card |
https://repository.kpfu.ru/eng/?p_id=127004&p_lang=2 |
Full metadata record |
Field DC |
Value |
Language |
dc.contributor.author |
Linkina Larisa Igorevna |
ru_RU |
dc.contributor.author |
Petrova Elena Vitalevna |
ru_RU |
dc.date.accessioned |
2014-01-01T00:00:00Z |
ru_RU |
dc.date.available |
2014-01-01T00:00:00Z |
ru_RU |
dc.date.issued |
2014 |
ru_RU |
dc.identifier.citation |
E. Petrova, L. Linkina To the Question of boundaries and composition of Gelasian Stratum in the Middle Volga Region / THE QUATERNARY OF THE URALS: global trends and Pan-European Quaternary records Ekaterinburg, Russia September 10–16, 2014 Ekaterinburg UrFU 2014 International conference INQUA-SEQS 2014. Р. 113-115.
|
ru_RU |
dc.identifier.uri |
https://repository.kpfu.ru/eng/?p_id=127004&p_lang=2 |
ru_RU |
dc.description.abstract |
THE QUATERNARY OF THE URALS: global trends and Pan-European Quaternary records |
ru_RU |
dc.description.abstract |
According to the ICS Resolution dated 2012 [1] the time interval of a quaternary system is widened up to 2,6 million years; the Gelasian Stratum was included to the quaternary system as the lower subdivision of Eopleistocene. According to the time period Chistopolian, Akkulaevian, and Biklyanian substages conventionally are related to the Gelasian Stage within the Middle Volga Region. Thus, nowadays the conventional lower boundary between Neogene and quaternary systems lies between regional subdivisions: Sokolian and Chistopolian substages, which earlier belonged to the unified Akchagyl regio-stage of the Neogene system. The upper boundary of Gelasian stratum is between Biklyanian and Omarian substages, which form the unified complex of depositions, sediments? accumulation of which occurred on the period of Akchagylian basin regression. |
ru_RU |
dc.language.iso |
ru |
ru_RU |
dc.subject |
quaternary system |
ru_RU |
dc.subject |
Gelasian Stratum |
ru_RU |
dc.subject |
Akchagyl regio-stage |
ru_RU |
dc.subject |
Middle Volga Region. |
ru_RU |
dc.title |
To the Question of boundaries and composition of Gelasian Stratum in the Middle Volga Region |
ru_RU |
dc.type |
Conference proceedings in Russian journals and collections |
ru_RU |
|