| Форма представления | Статьи в зарубежных журналах и сборниках |
| Год публикации | 2014 |
| Язык | русский |
|
Еснин Алексей Александрович, автор
Кольчугин Антон Николаевич, автор
Королев Эдуард Анатольевич, автор
Морозов Владимир Петрович, автор
|
| Библиографическое описание на языке оригинала |
Kolchugin A.N., Morozov V.P., Korolev E.A., Eskin A.A. Carbonate formation of the Lower Carboniferous in central part Volga–Ural basin // Current science, 2014, 107 (12), pp. 2029-2035. |
| Аннотация |
Carbonate rocks of the Lower Carboniferous (Tournaisian stage) of the central part Volga-Ural basin (the eastern portion of the East -European platform) have is of practical and scientific interests among to geologists, particularly because they containit contains large reserves of oil. These layersSuch layers have been researched by many geologists and, and accordingly they have been they were the subject of discussed in numerous many publications. However, many various problems questions, such as the creation sedimentation scheme of the rocks rock, are not solvedhave not been answered. We tried attempted to solve this problemresolve this particularly question by using a wealth of factual core material. The main methods of research were involved the structural and geneticalally analysis of rocks, in addition to which we used faciafacial reconstructions. The rocks are mainly represented in main by different types of shallow- water limestone. |
| Ключевые слова |
Volga-Ural region, Tournaisian stage, limestone, sedimentation, seabed topography, wave base level, prospects of oil |
| Название журнала |
Current Science
|
| Пожалуйста, используйте этот идентификатор, чтобы цитировать или ссылаться на эту карточку |
https://repository.kpfu.ru/?p_id=114331 |
Полная запись метаданных  |
| Поле DC |
Значение |
Язык |
| dc.contributor.author |
Еснин Алексей Александрович |
ru_RU |
| dc.contributor.author |
Кольчугин Антон Николаевич |
ru_RU |
| dc.contributor.author |
Королев Эдуард Анатольевич |
ru_RU |
| dc.contributor.author |
Морозов Владимир Петрович |
ru_RU |
| dc.date.accessioned |
2014-01-01T00:00:00Z |
ru_RU |
| dc.date.available |
2014-01-01T00:00:00Z |
ru_RU |
| dc.date.issued |
2014 |
ru_RU |
| dc.identifier.citation |
Kolchugin A.N., Morozov V.P., Korolev E.A., Eskin A.A. Carbonate formation of the Lower Carboniferous in central part Volga–Ural basin // Current science, 2014, 107 (12), pp. 2029-2035. |
ru_RU |
| dc.identifier.uri |
https://repository.kpfu.ru/?p_id=114331 |
ru_RU |
| dc.description.abstract |
Current Science |
ru_RU |
| dc.description.abstract |
Carbonate rocks of the Lower Carboniferous (Tournaisian stage) of the central part Volga-Ural basin (the eastern portion of the East -European platform) have is of practical and scientific interests among to geologists, particularly because they containit contains large reserves of oil. These layersSuch layers have been researched by many geologists and, and accordingly they have been they were the subject of discussed in numerous many publications. However, many various problems questions, such as the creation sedimentation scheme of the rocks rock, are not solvedhave not been answered. We tried attempted to solve this problemresolve this particularly question by using a wealth of factual core material. The main methods of research were involved the structural and geneticalally analysis of rocks, in addition to which we used faciafacial reconstructions. The rocks are mainly represented in main by different types of shallow- water limestone. |
ru_RU |
| dc.language.iso |
ru |
ru_RU |
| dc.subject |
Volga-Ural region |
ru_RU |
| dc.subject |
Tournaisian stage |
ru_RU |
| dc.subject |
limestone |
ru_RU |
| dc.subject |
sedimentation |
ru_RU |
| dc.subject |
seabed topography |
ru_RU |
| dc.subject |
wave base level |
ru_RU |
| dc.subject |
prospects of oil |
ru_RU |
| dc.title |
Carbonate formation of the Lower Carboniferous in central part Volga–Ural basin |
ru_RU |
| dc.type |
Статьи в зарубежных журналах и сборниках |
ru_RU |
|
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