KFU. Card publication. ACCESSORY MINERALIZATION OF DOLOMITE RESERVOIRS AS THE FACTOR OF FLUIDS VARIABILITY COMPOSITION

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FEDERAL UNIVERSITY

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ACCESSORY MINERALIZATION OF DOLOMITE RESERVOIRS AS THE FACTOR OF FLUIDS VARIABILITY COMPOSITION

Form of presentation

Articles in international journals and collections

Year of publication

2017

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Authors, employees of KFU

Eskin Aleksey Aleksandrovich, author

Bibliographic description in the original language

ESKIN A.A. ACCESSORY MINERALIZATION OF DOLOMITE RESERVOIRS AS THE FACTOR OF FLUIDS VARIABILITY COMPOSITION / A.A. ESKIN, E.A KOROLEV, A.I. BAKHTIN, A.N. KOLCHUGIN, E.R. BARIEVA // SGEM2017 Conference Proceedings (29 June - 5 July), 2017. - Vol. 17, Issue 11. - 11-18 pp

Annotation

17th International Multidisciplinary Scientific GeoConference SGEM 2017

Keywords

dolomites, accessory minerals, quartz, microcline, siderite, pyrite

The name of the journal

17th International Multidisciplinary Scientific GeoConference SGEM 2017

URL

https://sgemworld.at/sgemlib/spip.php?article8879&lang=en

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

https://repository.kpfu.ru/eng/?p_id=165886&p_lang=2

Full metadata record

Field DC	Value	Language
dc.contributor.author	Eskin Aleksey Aleksandrovich	ru_RU
dc.date.accessioned	2017-01-01T00:00:00Z	ru_RU
dc.date.available	2017-01-01T00:00:00Z	ru_RU
dc.date.issued	2017	ru_RU
dc.identifier.citation	ESKIN A.A. ACCESSORY MINERALIZATION OF DOLOMITE RESERVOIRS AS THE FACTOR OF FLUIDS VARIABILITY COMPOSITION / A.A. ESKIN, E.A KOROLEV, A.I. BAKHTIN, A.N. KOLCHUGIN, E.R. BARIEVA // SGEM2017 Conference Proceedings (29 June - 5 July), 2017. - Vol. 17, Issue 11. - 11-18 pp	ru_RU
dc.identifier.uri	https://repository.kpfu.ru/eng/?p_id=165886&p_lang=2	ru_RU
dc.description.abstract	17th International Multidisciplinary Scientific GeoConference SGEM 2017	ru_RU
dc.description.abstract	Oil-saturated Visean dolomite reservoirs were studied from the Tatarstan Republic, east of Russian platform. The main methods of study were X-ray and SEM analysis. Dolomite forms interstratified dense and porous layers with thickness of 0.5-4.0 m in oil-saturated parts of reservoirs. The dolomites are characterized by rhombic form of crystals. Many of them have crystal growth zones as alternate micro-layers with different iron content. In the pore space of dense dolomites find some iron accessory minerals such as siderite and pyrite. There are accessory crystals of quartz and aggregates of microcline in cavernous of porosity dolomites. Based on the heterogeneous composition of dolomites and their accessory minerals associations were modeled stages and hydrochemical parameters variation of fluids before oil charge.	ru_RU
dc.language.iso	ru	ru_RU
dc.subject	dolomites	ru_RU
dc.subject	accessory minerals	ru_RU
dc.subject	quartz	ru_RU
dc.subject	microcline	ru_RU
dc.subject	siderite	ru_RU
dc.subject	pyrite	ru_RU
dc.title	ACCESSORY MINERALIZATION OF DOLOMITE RESERVOIRS AS THE FACTOR OF FLUIDS VARIABILITY COMPOSITION	ru_RU
dc.type	Articles in international journals and collections	ru_RU