KFU. Card publication. Transformation of sandbody geometry as the result of enclosing clay rock compaction

KAZAN
FEDERAL UNIVERSITY

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TRANSFORMATION OF SANDBODY GEOMETRY AS THE RESULT OF ENCLOSING CLAY ROCK COMPACTION

Form of presentation

Articles in international journals and collections

Year of publication

2016

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Authors, employees of KFU

Valeeva Svetlana Evgenevna, author

Uspenskiy Boris Vadimovich, author

Bibliographic description in the original language

Valeeva, S.E. Transformation of sandbody geometry as the result of enclosing clay rock compaction / S.E. Valeeva, B.V. Uspensky // International Journal of Pharmacy and Technology. - 2016. - Volume 8, Issue 1. - Pages 11297-11305

Annotation

During paleogeographic studies the identification of channel, deltaic and avandeltaic environments of sedimentation is obstructed. Experience shows that their definition according to the granulometric composition of constituent deposits is not a sufficient basis for the reference to the category of continental facies. To do this, we should attract some indirect evidence, for example, the drawing of paleo drain network, the geometry of sandbodies and the configuration of basal and lateral contacts, etc. The performed studies demonstrated the transformation of sandbodies due to the nonuniform compressibility of clay and sand rocks, causing to the formation of various pseudo-structural elements in the form of bends and folds. Therefore, during the identification of formation conditions for clastic natural reservoirs the adjustment of trap forms is needed for the processes of enclosing clay rock compaction.

Keywords

sedimentation terms, sandstone pack, alluvial-deltaic formations, hydrocarbon traps

The name of the journal

International journal of Pharmacy and Technology

URL

http://www.ijptonline.com/wp-content/uploads/2016/04/11297-11305.pdf

Please use this ID to quote from or refer to the card

https://repository.kpfu.ru/eng/?p_id=146568&p_lang=2

Resource files

File name	Size (MB)	Format
11297_11305.pdf	0,61	pdf	show / download

Full metadata record

Field DC	Value	Language
dc.contributor.author	Valeeva Svetlana Evgenevna	ru_RU
dc.contributor.author	Uspenskiy Boris Vadimovich	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	Valeeva, S.E. Transformation of sandbody geometry as the result of enclosing clay rock compaction / S.E. Valeeva, B.V. Uspensky // International Journal of Pharmacy and Technology. - 2016. - Volume 8, Issue 1. - Pages 11297-11305	ru_RU
dc.identifier.uri	https://repository.kpfu.ru/eng/?p_id=146568&p_lang=2	ru_RU
dc.description.abstract	International journal of Pharmacy and Technology	ru_RU
dc.description.abstract	During paleogeographic studies the identification of channel, deltaic and avandeltaic environments of sedimentation is obstructed. Experience shows that their definition according to the granulometric composition of constituent deposits is not a sufficient basis for the reference to the category of continental facies. To do this, we should attract some indirect evidence, for example, the drawing of paleo drain network, the geometry of sandbodies and the configuration of basal and lateral contacts, etc. The performed studies demonstrated the transformation of sandbodies due to the nonuniform compressibility of clay and sand rocks, causing to the formation of various pseudo-structural elements in the form of bends and folds. Therefore, during the identification of formation conditions for clastic natural reservoirs the adjustment of trap forms is needed for the processes of enclosing clay rock compaction.	ru_RU
dc.language.iso	ru	ru_RU
dc.subject	sedimentation terms	ru_RU
dc.subject	sandstone pack	ru_RU
dc.subject	alluvial-deltaic formations	ru_RU
dc.subject	hydrocarbon traps	ru_RU
dc.title	Transformation of sandbody geometry as the result of enclosing clay rock compaction	ru_RU
dc.type	Articles in international journals and collections	ru_RU