КФУ. Карточка публикации. Sedimentological review of upper triassic (Mulussa F formation) in Euphrates-Graben Syria

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SEDIMENTOLOGICAL REVIEW OF UPPER TRIASSIC (MULUSSA F FORMATION) IN EUPHRATES-GRABEN SYRIA

Форма представления

Статьи в зарубежных журналах и сборниках

Год публикации

2016

Язык

английский

Авторы, сотрудники КФУ

Морозов Владимир Петрович, автор

Юсеф Ибрахем , автор

Библиографическое описание на языке оригинала

Yousef I, Morozov V, Al-Kadi M., Sedimentological review of upper triassic (Mulussa F formation) in Euphrates-Graben Syria//Journal of Engineering and Applied Sciences. - 2016. - Vol.11, Is.14. - P.3067-3079.

Аннотация

Mulussa F foпnation is one of the important geological foпnations constituting the Mulussa group in Syria. The objective of this research is to review of sediments Mulussa F foпnation. Its deposits contain almost 50% of hydrocarbon potential through Euphrates Graben. Boreholes data peпnitted confining the foпnation between two Lithostratigraphic markers and enaЫed its division into three Lithostratigraphic members J\1UF3, J\1UF2, J\1UF1 (from bottom to top). Each member consists of а set of шrits, subшrits and lithologic intervals. Petrology studying provides а precise petrological description of various foпnation members and their Digenetic. Results show that the members of the structшe are composed of continental detrital sediments made up of clay stones (Kaolinite/Illite) and Shale/Dolomitic claystone, covered Ьу intervals of quartz sandstones, clay sandstones, and silt sandstones. The carbonate sediments are absent from the foпnation Illite it's base which consists of Dolomitic claystone and its top which are close to carbonate composition. This sediment of those members spread out as repeated or hannonic alterations whose faces gradients reflect transgression and regression sequences. Due to the historical value of Mulussa F foпnation, it is vital to investigate its sediment status. The study of these sediments leads to represent naпow baпiers near river mouth with meandering channels and limited coastal deposits.

Ключевые слова

Euphrates Graben, Triassic, Mulussa F, stratigraphy, sedimentology, chemostratigraphy

Название журнала

Journal of Engineering and Applied Sciences

URL

https://www.scopus.com/inward/record.url?eid=2-s2.0-85014737286&partnerID=40&md5=27ef5861ebd4252497d4fd995b1e3c28

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https://repository.kpfu.ru/?p_id=188279

Полная запись метаданных

Поле DC	Значение	Язык
dc.contributor.author	Морозов Владимир Петрович	ru_RU
dc.contributor.author	Юсеф Ибрахем	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	Yousef I, Morozov V, Al-Kadi M., Sedimentological review of upper triassic (Mulussa F formation) in Euphrates-Graben Syria//Journal of Engineering and Applied Sciences. - 2016. - Vol.11, Is.14. - P.3067-3079.	ru_RU
dc.identifier.uri	https://repository.kpfu.ru/?p_id=188279	ru_RU
dc.description.abstract	Journal of Engineering and Applied Sciences	ru_RU
dc.description.abstract	Mulussa F foпnation is one of the important geological foпnations constituting the Mulussa group in Syria. The objective of this research is to review of sediments Mulussa F foпnation. Its deposits contain almost 50% of hydrocarbon potential through Euphrates Graben. Boreholes data peпnitted confining the foпnation between two Lithostratigraphic markers and enaЫed its division into three Lithostratigraphic members J\1UF3, J\1UF2, J\1UF1 (from bottom to top). Each member consists of а set of шrits, subшrits and lithologic intervals. Petrology studying provides а precise petrological description of various foпnation members and their Digenetic. Results show that the members of the structшe are composed of continental detrital sediments made up of clay stones (Kaolinite/Illite) and Shale/Dolomitic claystone, covered Ьу intervals of quartz sandstones, clay sandstones, and silt sandstones. The carbonate sediments are absent from the foпnation Illite it's base which consists of Dolomitic claystone and its top which are close to carbonate composition. This sediment of those members spread out as repeated or hannonic alterations whose faces gradients reflect transgression and regression sequences. Due to the historical value of Mulussa F foпnation, it is vital to investigate its sediment status. The study of these sediments leads to represent naпow baпiers near river mouth with meandering channels and limited coastal deposits.	ru_RU
dc.language.iso	ru	ru_RU
dc.subject	Euphrates Graben	ru_RU
dc.subject	Triassic	ru_RU
dc.subject	Mulussa F	ru_RU
dc.subject	stratigraphy	ru_RU
dc.subject	sedimentology	ru_RU
dc.subject	chemostratigraphy	ru_RU
dc.title	Sedimentological review of upper triassic (Mulussa F formation) in Euphrates-Graben Syria	ru_RU
dc.type	Статьи в зарубежных журналах и сборниках	ru_RU