KFU. Card publication. DIAGENETIC CHLORITE, ILLITE AND ILLITE-SMECTITE MINERALS IN SANDSTONE RESERVOIR; STRUCTURAL, MORPHOLOGY AND PRECIPITATION UPPER TRIASSIC RESERVOIR, SYRIA

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DIAGENETIC CHLORITE, ILLITE AND ILLITE-SMECTITE MINERALS IN SANDSTONE RESERVOIR; STRUCTURAL, MORPHOLOGY AND PRECIPITATION UPPER TRIASSIC RESERVOIR, SYRIA

Form of presentation

Articles in international journals and collections

Year of publication

2017

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Authors, employees of KFU

Morozov Vladimir Petrovich, author

Usmanov Sergey Anatolevich, author

Yusef Ibrakhem , author

Bibliographic description in the original language

Ibrahim Yousef., Sergey Usmanov., Vladimir Morozov., Marat Validov. DIAGENETIC CHLORITE, ILLITE AND ILLITE-SMECTITE MINERALS IN SANDSTONE RESERVOIR; STRUCTURAL, MORPHOLOGY AND PRECIPITATION UPPER TRIASSIC RESERVOIR, SYRIA//International Multidisciplinary Scientific GeoConference Surveying Geology and Mining Ecology Management, SGEM. - 2017. - Vol.17, Is.15. - P.115-124.

Annotation

The purpose of this article is to discuss the authigenic chlorite, illite and illite-smectite mixed layers at the sandstone of upper Triassic reservoir at Euphrates graben fields east of Syria related to their structural, morphology and diagenetic events and precipitation. The upper Triassic sandstone reservoir is one of the most important oil and gas reservoirs at the east of Syria; it contains about 60 % of the total hydrocarbon volume at the area. Petrographical analyses combined with the different core analysis using polarized, scanning electron microscope (SEM) analysis, X-ray diffraction (XRD) and energy dispersive X-ray spectrometry (EDS) system have been used in this article. The upper Triassic sandstones are typically of quartz arenite; detrital quartz is the dominant phase (mean 74%). The authigenic clay minerals of this reservoir are dominated by kaolinite, chlorite, illite, and illite-smectite mixture. Authigenic chlorites are found in range from traces to ~13%, most of the chlorite in the form of overgrowth and cover the detrital grains. Authigenic illite found in traces to ~4% of the whole rock sample, while the illite-smectite mixture layers are found in trac-es~7%. Both of illite, and illite-smectite mixture are 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. The different analyses indicate the illite and illite-smectite mixture are precipitated durial deep burial diagenesis.

Keywords

diagenetic, chlorite, kaolinite, illite, sandstone, upper Triassic, Syria

The name of the journal

International Multidisciplinary Scientific GeoConference Surveying Geology and Mining Ecology Management, SGEM

URL

https://www.scopus.com/inward/record.uri?eid=2-s2.0-85063095148&doi=10.5593%2fsgem2017H%2f15%2fS06.015&partnerID=40&md5=e73da6cfc2a74c255083e3f92dd65d6d

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

https://repository.kpfu.ru/eng/?p_id=216892&p_lang=2

Full metadata record

Field DC	Value	Language
dc.contributor.author	Morozov Vladimir Petrovich	ru_RU
dc.contributor.author	Usmanov Sergey Anatolevich	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	Ibrahim Yousef., Sergey Usmanov., Vladimir Morozov., Marat Validov. DIAGENETIC CHLORITE, ILLITE AND ILLITE-SMECTITE MINERALS IN SANDSTONE RESERVOIR; STRUCTURAL, MORPHOLOGY AND PRECIPITATION UPPER TRIASSIC RESERVOIR, SYRIA//International Multidisciplinary Scientific GeoConference Surveying Geology and Mining Ecology Management, SGEM. - 2017. - Vol.17, Is.15. - P.115-124.	ru_RU
dc.identifier.uri	https://repository.kpfu.ru/eng/?p_id=216892&p_lang=2	ru_RU
dc.description.abstract	International Multidisciplinary Scientific GeoConference Surveying Geology and Mining Ecology Management, SGEM	ru_RU
dc.description.abstract	The purpose of this article is to discuss the authigenic chlorite, illite and illite-smectite mixed layers at the sandstone of upper Triassic reservoir at Euphrates graben fields east of Syria related to their structural, morphology and diagenetic events and precipitation. The upper Triassic sandstone reservoir is one of the most important oil and gas reservoirs at the east of Syria; it contains about 60 % of the total hydrocarbon volume at the area. Petrographical analyses combined with the different core analysis using polarized, scanning electron microscope (SEM) analysis, X-ray diffraction (XRD) and energy dispersive X-ray spectrometry (EDS) system have been used in this article. The upper Triassic sandstones are typically of quartz arenite; detrital quartz is the dominant phase (mean 74%). The authigenic clay minerals of this reservoir are dominated by kaolinite, chlorite, illite, and illite-smectite mixture. Authigenic chlorites are found in range from traces to ~13%, most of the chlorite in the form of overgrowth and cover the detrital grains. Authigenic illite found in traces to ~4% of the whole rock sample, while the illite-smectite mixture layers are found in trac-es~7%. Both of illite, and illite-smectite mixture are 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. The different analyses indicate the illite and illite-smectite mixture are precipitated durial deep burial diagenesis.	ru_RU
dc.language.iso	ru	ru_RU
dc.subject	diagenetic	ru_RU
dc.subject	chlorite	ru_RU
dc.subject	kaolinite	ru_RU
dc.subject	illite	ru_RU
dc.subject	sandstone	ru_RU
dc.subject	upper Triassic	ru_RU
dc.subject	Syria	ru_RU
dc.title	DIAGENETIC CHLORITE, ILLITE AND ILLITE-SMECTITE MINERALS IN SANDSTONE RESERVOIR; STRUCTURAL, MORPHOLOGY AND PRECIPITATION UPPER TRIASSIC RESERVOIR, SYRIA	ru_RU
dc.type	Articles in international journals and collections	ru_RU