KFU. Card publication. Learning environments paleogeographic situations in early Permian time based on preliminary magneto-mineralogical investigations in the exposure Dal?ny Tyulkas (Republic of Bashkortostan)

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LEARNING ENVIRONMENTS PALEOGEOGRAPHIC SITUATIONS IN EARLY PERMIAN TIME BASED ON PRELIMINARY MAGNETO-MINERALOGICAL INVESTIGATIONS IN THE EXPOSURE DAL?NY TYULKAS (REPUBLIC OF BASHKORTOSTAN)

Form of presentation

International monographs

Year of publication

2017

Authors, employees of KFU

Kosareva Lina Raisovna, author

Sungatullina Guzal Marsovna, author

Authors, students KFU

Yakunina Polina Georgievna, author

Bibliographic description in the original language

The analysis of Permian climate and paleogeography can be useful in forecasting of the situation in the future. The exposure characterized the boundary between the Sakmarian and Artinian tiers and represented by intercalation of argillites, siltstones, clays, limestones and sandstones. The paleogeographic studies are conducted with application of magnetic methods. The collection of 24 samples has been selected for carrying out the laboratory magnetic and mineralogical analysis. The complex of methods includes measurements of a magnetic susceptibility, hysteresis methods. The Sakmara stage is characterized by stability of a magnetic susceptibility and remanence coercivity. Throughout an artinsky century the mode of sedimentation is fluctuate because climatic changes have influenced on different nature processes. A possible cause of such changes is the decrease in sea level due to mountain collision. Climate system tended to be more warming with full degradation of the Gondwana glaciatio

Please use this ID to quote from or refer to the card

https://repository.kpfu.ru/eng/?p_id=202311&p_lang=2

Full metadata record

Field DC	Value	Language
dc.contributor.author	Kosareva Lina Raisovna	ru_RU
dc.contributor.author	Sungatullina Guzal Marsovna	ru_RU
dc.contributor.author	Yakunina Polina Georgievna	ru_RU
dc.date.accessioned	2017-01-01T00:00:00Z	ru_RU
dc.date.available	2017-01-01T00:00:00Z	ru_RU
dc.date.issued	2017	ru_RU
dc.identifier.citation	The analysis of Permian climate and paleogeography can be useful in forecasting of the situation in the future. The exposure characterized the boundary between the Sakmarian and Artinian tiers and represented by intercalation of argillites, siltstones, clays, limestones and sandstones. The paleogeographic studies are conducted with application of magnetic methods. The collection of 24 samples has been selected for carrying out the laboratory magnetic and mineralogical analysis. The complex of methods includes measurements of a magnetic susceptibility, hysteresis methods. The Sakmara stage is characterized by stability of a magnetic susceptibility and remanence coercivity. Throughout an artinsky century the mode of sedimentation is fluctuate because climatic changes have influenced on different nature processes. A possible cause of such changes is the decrease in sea level due to mountain collision. Climate system tended to be more warming with full degradation of the Gondwana glaciatio	ru_RU
dc.identifier.uri	https://repository.kpfu.ru/eng/?p_id=202311&p_lang=2	ru_RU
dc.language.iso	ru	ru_RU
dc.title	Learning environments paleogeographic situations in early Permian time based on preliminary magneto-mineralogical investigations in the exposure Dal?ny Tyulkas (Republic of Bashkortostan)	ru_RU
dc.type	International monographs	ru_RU