Form of presentation | Articles in international journals and collections |
Year of publication | 2016 |
Язык | английский |
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Khasanov Rinat Radikovich, author
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Mullakaev Almaz Ilyasovich, postgraduate kfu
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Bibliographic description in the original language |
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 |
Annotation |
16th International Multidisciplinary Scientific GeoConference SGEM 2016 |
Keywords |
paleogeography, Permian reservoir rocks, bitumen, deposits |
The name of the journal |
16th International Multidisciplinary Scientific GeoConference SGEM 2016
|
Please use this ID to quote from or refer to the card |
https://repository.kpfu.ru/eng/?p_id=133129&p_lang=2 |
Full metadata record ![](https://shelly.kpfu.ru/pdf/picture/arrow_black_right.gif) |
Field DC |
Value |
Language |
dc.contributor.author |
Khasanov Rinat Radikovich |
ru_RU |
dc.contributor.author |
Mullakaev Almaz Ilyasovich |
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/eng/?p_id=133129&p_lang=2 |
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 |
Articles in international journals and collections |
ru_RU |
|