| Форма представления | Статьи в зарубежных журналах и сборниках |
| Год публикации | 2018 |
| Язык | английский |
|
Муллакаев Алмаз Ильясович, автор
|
| Библиографическое описание на языке оригинала |
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. |
| Аннотация |
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. |
| Ключевые слова |
bitumen sands, bitumen sandstones, Permian bitumen, tar sands, genesis, Aeolian sediments |
| Название журнала |
IOP Conference Series: Earth and Environmental Science
|
| URL |
http://www.filodirittoeditore.com/index.php?route=product/product&product_id=160 |
| Пожалуйста, используйте этот идентификатор, чтобы цитировать или ссылаться на эту карточку |
https://repository.kpfu.ru/?p_id=184183 |
Полная запись метаданных  |
| Поле DC |
Значение |
Язык |
| dc.contributor.author |
Муллакаев Алмаз Ильясович |
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/?p_id=184183 |
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 |
Статьи в зарубежных журналах и сборниках |
ru_RU |
|
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