KFU. Card publication. The Aeolian factor in the formation of the Sheshmian Horizon sands and sandstones in the Permian of the South-Tatar Arch

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THE AEOLIAN FACTOR IN THE FORMATION OF THE SHESHMIAN HORIZON SANDS AND SANDSTONES IN THE PERMIAN OF THE SOUTH-TATAR ARCH

Form of presentation

Articles in international journals and collections

Year of publication

2018

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Authors, employees of KFU

Mullakaev Almaz Ilyasovich, author

Bibliographic description in the original language

Mullakaev Almaz, Khasanov Rinat. The Aeolian factor in the formation of the Sheshmian Horizon sands and sandstones in the Permian of the South-Tatar Arch / In book: Barclay, M., Nikolaeva, S., Silantiev, V. (Eds.) Kazan Golovkinsky Stratigraphic Meeting, 2017: Advances in Devonian, Carboniferous and Permian Research: Stratigraphy, Environments, Climate and Resources. Filodiritto International Proceedings, Bologna, Italy, pp. 381-385.

Annotation

Since the beginning of the exploitation of high-viscosity oil fields, interest in the study of bituminous sands and sandstones of the Sheshmian horizon (Cisuralian, Ufimian Stage of the General Stratigraphic Scale of Russia) has increased. Bitumen deposits are associated with terrigenous-clastic rocks with high reservoir properties, due to the composition, structural and texture features of the rocks. The main characteristic features of such rocks are formed at the stage of sedimentation under the influence of primary sedimentary factors. The Sheshmian horizon has a two-layered structure and is characterized by the presence of two layers that differ in composition. Features of the composition of sand and sandstone layers can be due to the influence of various factors in the process of their formation.

Keywords

bitumen sands, bitumen sandstones, Permian bitumen, tar sands, genesis, Aeolian sediments

The name of the journal

IOP Conference Series: Earth and Environmental Science

URL

http://www.filodirittoeditore.com/index.php?route=product/product&product_id=160

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

https://repository.kpfu.ru/eng/?p_id=184183&p_lang=2

Full metadata record

Field DC	Value	Language
dc.contributor.author	Mullakaev Almaz Ilyasovich	ru_RU
dc.date.accessioned	2018-01-01T00:00:00Z	ru_RU
dc.date.available	2018-01-01T00:00:00Z	ru_RU
dc.date.issued	2018	ru_RU
dc.identifier.citation	Mullakaev Almaz, Khasanov Rinat. The Aeolian factor in the formation of the Sheshmian Horizon sands and sandstones in the Permian of the South-Tatar Arch / In book: Barclay, M., Nikolaeva, S., Silantiev, V. (Eds.) Kazan Golovkinsky Stratigraphic Meeting, 2017: Advances in Devonian, Carboniferous and Permian Research: Stratigraphy, Environments, Climate and Resources. Filodiritto International Proceedings, Bologna, Italy, pp. 381-385.	ru_RU
dc.identifier.uri	https://repository.kpfu.ru/eng/?p_id=184183&p_lang=2	ru_RU
dc.description.abstract	IOP Conference Series: Earth and Environmental Science	ru_RU
dc.description.abstract	Since the beginning of the exploitation of high-viscosity oil fields, interest in the study of bituminous sands and sandstones of the Sheshmian horizon (Cisuralian, Ufimian Stage of the General Stratigraphic Scale of Russia) has increased. Bitumen deposits are associated with terrigenous-clastic rocks with high reservoir properties, due to the composition, structural and texture features of the rocks. The main characteristic features of such rocks are formed at the stage of sedimentation under the influence of primary sedimentary factors. The Sheshmian horizon has a two-layered structure and is characterized by the presence of two layers that differ in composition. Features of the composition of sand and sandstone layers can be due to the influence of various factors in the process of their formation.	ru_RU
dc.language.iso	ru	ru_RU
dc.subject	bitumen sands	ru_RU
dc.subject	bitumen sandstones	ru_RU
dc.subject	Permian bitumen	ru_RU
dc.subject	tar sands	ru_RU
dc.subject	genesis	ru_RU
dc.subject	Aeolian sediments	ru_RU
dc.title	The Aeolian factor in the formation of the Sheshmian Horizon sands and sandstones in the Permian of the South-Tatar Arch	ru_RU
dc.type	Articles in international journals and collections	ru_RU