Form of presentation | Articles in international journals and collections |
Year of publication | 2014 |
Язык | русский |
|
Esnin Aleksey Aleksandrovich, author
Kolchugin Anton Nikolaevich, author
Korolev Eduard Anatolevich, author
Morozov Vladimir Petrovich, author
|
Bibliographic description in the original language |
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. |
Annotation |
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. |
Keywords |
Volga-Ural region, Tournaisian stage, limestone, sedimentation, seabed topography, wave base level, prospects of oil |
The name of the journal |
Current Science
|
Please use this ID to quote from or refer to the card |
https://repository.kpfu.ru/eng/?p_id=114331&p_lang=2 |
Full metadata record |
Field DC |
Value |
Language |
dc.contributor.author |
Esnin Aleksey Aleksandrovich |
ru_RU |
dc.contributor.author |
Kolchugin Anton Nikolaevich |
ru_RU |
dc.contributor.author |
Korolev Eduard Anatolevich |
ru_RU |
dc.contributor.author |
Morozov Vladimir Petrovich |
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/eng/?p_id=114331&p_lang=2 |
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 |
Articles in international journals and collections |
ru_RU |
|