KFU. Card publication. AUTHIGENIC KAOLINITE AND ILLITE CHARACTERISTICS IN THE UPPER TRIASSIC SANDSTONE RESERVOIR (EUPHRATES GRABEN FIELDS, EAST SYRIA)

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AUTHIGENIC KAOLINITE AND ILLITE CHARACTERISTICS IN THE UPPER TRIASSIC SANDSTONE RESERVOIR (EUPHRATES GRABEN FIELDS, EAST SYRIA)

Form of presentation

Articles in Russian journals and collections

Year of publication

2017

Authors, employees of KFU

Morozov Vladimir Petrovich, author

Authors, postgraduates KFU

Yusef Ibrakhem , postgraduate kfu

Bibliographic description in the original language

AUTHIGENIC KAOLINITE AND ILLITE CHARACTERISTICS IN THE UPPER TRIASSIC SANDSTONE RESERVOIR (EUPHRATES GRABEN FIELDS, EAST SYRIA)

Annotation

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Keywords

Authigenic, kaolinite, illite, Euphrates graben, upper Triassic, Syria.

Place of publication

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The name of the journal

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Publishing house

420008, ��, ��. ��,18, �� , �. 068

URL

http://kpfu.ru/uz-eng/hum/contact-us, Phone: +7(843) 233-73-01 E-mail: uz.ku@kpfu.ru

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

https://repository.kpfu.ru/eng/?p_id=165473&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	AUTHIGENIC KAOLINITE AND ILLITE CHARACTERISTICS IN THE UPPER TRIASSIC SANDSTONE RESERVOIR (EUPHRATES GRABEN FIELDS, EAST SYRIA)	ru_RU
dc.identifier.uri	https://repository.kpfu.ru/eng/?p_id=165473&p_lang=2	ru_RU
dc.description.abstract	��	ru_RU
dc.description.abstract	��	ru_RU
dc.description.abstract	The upper Triassic sandstone reservoir (Mulussa F formation) is a main hydrocarbon target at the Syria Euphrates graben area. The experimental results; X-Ray Diffraction (XRD), Scanning Electron Microprobe (SEM) and Electron Diffraction System (EDS) analysis show that the clay minerals of this reservoir are dominated by kaolinite, illite, and illite-smectite mixture. Kaolinite is the main clay minerals phase found, morphologically, it?s rec-orded as hexagonal to pseudo hexagonal platelets or booklet; consist of particles clusters (10 to 15μm micrometre) of crystals arranged as sub to euhedral blocky structures often measure between 20 to 60 μm in length that partially or completely filled the pore spaces. Illite constitutes about 37 %, and identified as grain coating or pore filling phase composed of well-crystallized lath-like blades (10 μm), and short fiber-like morphology partially filled the intergranular pore and has nucleated at the margins of detrital clay surfaces.	ru_RU
dc.language.iso	ru	ru_RU
dc.publisher	420008, ��, ��. ��,18, �� , �. 068	ru_RU
dc.subject	Authigenic	ru_RU
dc.subject	kaolinite	ru_RU
dc.subject	illite	ru_RU
dc.subject	Euphrates graben	ru_RU
dc.subject	upper Triassic	ru_RU
dc.subject	Syria.	ru_RU
dc.title	AUTHIGENIC KAOLINITE AND ILLITE CHARACTERISTICS IN THE UPPER TRIASSIC SANDSTONE RESERVOIR (EUPHRATES GRABEN FIELDS, EAST SYRIA)	ru_RU
dc.type	Articles in Russian journals and collections	ru_RU