КФУ. Карточка публикации. Paleogeographic factors of the formation of Permian reservoir rocks of bitumen deposits in the east of the Russian plate (Russia)

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PALEOGEOGRAPHIC FACTORS OF THE FORMATION OF PERMIAN RESERVOIR ROCKS OF BITUMEN DEPOSITS IN THE EAST OF THE RUSSIAN PLATE (RUSSIA)

Форма представления

Статьи в зарубежных журналах и сборниках

Год публикации

2016

Язык

английский

Авторы, сотрудники КФУ

Хасанов Ринат Радикович, автор

Авторы, аспиранты КФУ

Муллакаев Алмаз Ильясович, автор

Библиографическое описание на языке оригинала

Mullakaev A.I., Khasanov R.R. Paleogeographic factors of the formation of Permian reservoir rocks of bitumen deposits in the east of the Russian plate (Russia) /International Multidisciplinary Scientific GeoConference Surveying Geology and Mining Ecology Management, SGEM Volume 1, 2016, 469-474 pp. DOI: 10.5593/SGEM2016/B11/S01.059

Аннотация

16th International Multidisciplinary Scientific GeoConference SGEM 2016

Ключевые слова

paleogeography, Permian reservoir rocks, bitumen, deposits

Название журнала

16th International Multidisciplinary Scientific GeoConference SGEM 2016

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https://repository.kpfu.ru/?p_id=133129

Полная запись метаданных

Поле DC	Значение	Язык
dc.contributor.author	Хасанов Ринат Радикович	ru_RU
dc.contributor.author	Муллакаев Алмаз Ильясович	ru_RU
dc.date.accessioned	2016-01-01T00:00:00Z	ru_RU
dc.date.available	2016-01-01T00:00:00Z	ru_RU
dc.date.issued	2016	ru_RU
dc.identifier.citation	Mullakaev A.I., Khasanov R.R. Paleogeographic factors of the formation of Permian reservoir rocks of bitumen deposits in the east of the Russian plate (Russia) /International Multidisciplinary Scientific GeoConference Surveying Geology and Mining Ecology Management, SGEM Volume 1, 2016, 469-474 pp. DOI: 10.5593/SGEM2016/B11/S01.059	ru_RU
dc.identifier.uri	https://repository.kpfu.ru/?p_id=133129	ru_RU
dc.description.abstract	16th International Multidisciplinary Scientific GeoConference SGEM 2016	ru_RU
dc.description.abstract	At the Permian period in the east of Russian plate took place a change of sedimentation regimes, caused by changes in paleogeographic conditions. Among the Permian deposits there are various sedimentary formations, which were formed in different climates (evaporite sulfate-carbonate, coal-bearing, gray-colored marine sediments, red beds, etc.) Different types of minerals relate with them such as gypsum, coal, copper sandstones and shales, bitumen. Recently, interest to the bitumen is increased, because they are valuable multipurpose and multifunctional feedstock (fuel, oil, etc.). They have significant resources in the Permian sediments, which can range from 1.5 to 10 billion tons. Bitumen deposits belong to the sandstones of Ufimian (Kungurian ? ICS) stage (sheshminskiy horizon) of Permian period. Bituminous sandstones are cross-bedded, small- or medium-grained, polymictic. They locate at small depths from the surface up to 400 m. In spite of long-studying history of Permian deposits	ru_RU
dc.language.iso	ru	ru_RU
dc.subject	paleogeography	ru_RU
dc.subject	Permian reservoir rocks	ru_RU
dc.subject	bitumen	ru_RU
dc.subject	deposits	ru_RU
dc.title	Paleogeographic factors of the formation of Permian reservoir rocks of bitumen deposits in the east of the Russian plate (Russia)	ru_RU
dc.type	Статьи в зарубежных журналах и сборниках	ru_RU