КФУ. Карточка публикации. 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)

Форма представления

Зарубежные монографии

Год публикации

2017

Авторы, сотрудники КФУ

Косарева Лина Раисовна, автор

Сунгатуллина Гузаль Марсовна, автор

Авторы, студенты КФУ

Якунина Полина Георгиевна, автор

Библиографическое описание на языке оригинала

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

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https://repository.kpfu.ru/?p_id=202311

Полная запись метаданных

Поле DC	Значение	Язык
dc.contributor.author	Косарева Лина Раисовна	ru_RU
dc.contributor.author	Сунгатуллина Гузаль Марсовна	ru_RU
dc.contributor.author	Якунина Полина Георгиевна	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/?p_id=202311	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	Зарубежные монографии	ru_RU