KFU. Card publication. DIAGENETIC AND RESERVOIR QUALITY EVOLUTION OF UPPER TRIASSIC SANDSTONE, EUPHRATES GRABEN, EAST SYRIA

KAZAN
FEDERAL UNIVERSITY

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DIAGENETIC AND RESERVOIR QUALITY EVOLUTION OF UPPER TRIASSIC SANDSTONE, EUPHRATES GRABEN, EAST SYRIA

Form of presentation

Articles in international journals and collections

Year of publication

2017

Authors, employees of KFU

Morozov Vladimir Petrovich, author

Other authors

EL-KADI MOHAMMAD

Authors, postgraduates KFU

Yusef Ibrakhem , postgraduate kfu

Bibliographic description in the original language

DIAGENETIC AND RESERVOIR QUALITY EVOLUTION OF UPPER TRIASSIC SANDSTONE, EUPHRATES GRABEN, EAST SYRIA

Annotation

Jorunal of petrolume geology

Keywords

Diagenesis, reservoir, sandstone, upper Triassic, Euphrates graben, Syria.

Place of publication

The name of the journal

Jorunal of petrolume geology

Publishing house

Wiley Online Library, Journal of Petroleum Geology

URL

http://onlinelibrary.wiley.com/journal/10.1111/(ISSN)1747-5457

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

https://repository.kpfu.ru/eng/?p_id=165477&p_lang=2

Full metadata record

Field DC	Value	Language
dc.contributor.author	Morozov Vladimir Petrovich	ru_RU
dc.contributor.author	Yusef Ibrakhem	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	DIAGENETIC AND RESERVOIR QUALITY EVOLUTION OF UPPER TRIASSIC SANDSTONE, EUPHRATES GRABEN, EAST SYRIA	ru_RU
dc.identifier.uri	https://repository.kpfu.ru/eng/?p_id=165477&p_lang=2	ru_RU
dc.description.abstract	Jorunal of petrolume geology	ru_RU
dc.description.abstract	The upper Triassic sandstones are typically of quartz arenite; detrital quartz is the dominant phase (mean 74%). The authigenic minerals within the sandstones include quartz overgrowth (0.3~9%), kaolinite (traces~11%), chlorite (traces~13%), illite (traces~4%), illite-smectite mixture (traces~7%), dolomite (traces to 17%), siderite (traces to 23%), pyrite (traces to ~3%), anhydrite (traces~2%), barite (traces~6%), and anatase in traces amounts. The pore types recognized in the studied samples are intergranular pores, intragranular, oversized, micro-pores and fracture pores. The porosity values are ranges from 1% to 18% (with an average of 10%). The permeability values, ranging from 100 to 3880 millidarcy The diagenetic history of the upper Triassic sandstone has been greatly influenced by early diagenetic processes which included development of haematite, infiltration of detrital clay, precipitation of K-feldspar, precipitation of kaolinite, chlorite, pyrite, siderite, and anatase.	ru_RU
dc.language.iso	ru	ru_RU
dc.publisher	Wiley Online Library, Journal of Petroleum Geology	ru_RU
dc.subject	Diagenesis	ru_RU
dc.subject	reservoir	ru_RU
dc.subject	sandstone	ru_RU
dc.subject	upper Triassic	ru_RU
dc.subject	Euphrates graben	ru_RU
dc.subject	Syria.	ru_RU
dc.title	DIAGENETIC AND RESERVOIR QUALITY EVOLUTION OF UPPER TRIASSIC SANDSTONE, EUPHRATES GRABEN, EAST SYRIA	ru_RU
dc.type	Articles in international journals and collections	ru_RU