КФУ. Карточка публикации. STRUCTURAL SETTING AND ZONAL DISTRIBUTION OF UPPER TRIASSIC - LOWER CRETACEOUS RESERVOIRS IN THE SYRIAN EUPHRATES GRABEN

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STRUCTURAL SETTING AND ZONAL DISTRIBUTION OF UPPER TRIASSIC - LOWER CRETACEOUS RESERVOIRS IN THE SYRIAN EUPHRATES GRABEN

Форма представления

Статьи в зарубежных журналах и сборниках

Год публикации

2018

Язык

английский

Авторы, сотрудники КФУ

Морозов Владимир Петрович, автор

Судаков Владислав Анатольевич, автор

Юсеф Ибрахем , автор

Библиографическое описание на языке оригинала

Ibrahem Yousef., Vladislav Sudakov., Vladimir Morozov., El Kadi Mohammad. STRUCTURAL SETTING AND ZONAL DISTRIBUTION OF UPPER TRIASSIC - LOWER CRETACEOUS RESERVOIRS IN THE SYRIAN EUPHRATES GRABEN//International Multidisciplinary Scientific GeoConference Surveying Geology and Mining Ecology Management, SGEM. - 2018. - Vol.18, Is.1.4. - P.811-818.

Аннотация

The purpose of the article is to assess the regional structure of the upper Triassic - lower Cretaceous sediments (Mulussa F and Rutbah reservoirs), which serve as an important targets for hydrocarbons production and exploration to the center and Middle East of Syria. The upper Triassic - lower Cretaceous sediments are approximately of 800 m thickness consist mainly of floodplain clays interbedded with medium to fine grained fluvial sandstones. In addition, there are dolomites and clay dolomites present in the lower parts of these deposits. The upper Triassic - lower Cretaceous deposits at Euphrates graben area were affected by the tow unconformity erosions; BKL and BKU, which led to significant changes in the thickness of the reservoirs sediments. These changes in thickness are also controlled by the axis of the non-isometric depositional basin, which has a direction from the North-West to the South-East. Another factor controls the changes and distribution of the thickness of upper Triassic - lower Cretaceous zones sediments which are the presence of the two uplifts (Khleissia uplift to the North-East and Rutbah uplift to the South-West). The high thickness of the upper Triassic sediments in the central part of the Euphrates graben suggests that the graben structure was formed prior to the unconformities erosion; BKL and BKU. Lower Cretaceous deposits are preserved almost inside the entire graben with a greater thickness on the flanks of the North-East and South-West of the Euphrates graben axis.

Ключевые слова

Regional, upper Triassic, lower Cretaceous, Euphrates graben, Syria.

Название журнала

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

URL

https://www.scopus.com/inward/record.uri?eid=2-s2.0-85058871977&doi=10.5593%2fsgem2018%2f1.4%2fS06.106&partnerID=40&md5=616bfa449d5da4c933bdd622bc68faaa

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https://repository.kpfu.ru/?p_id=213569

Полная запись метаданных

Поле DC	Значение	Язык
dc.contributor.author	Морозов Владимир Петрович	ru_RU
dc.contributor.author	Судаков Владислав Анатольевич	ru_RU
dc.contributor.author	Юсеф Ибрахем	ru_RU
dc.date.accessioned	2018-01-01T00:00:00Z	ru_RU
dc.date.available	2018-01-01T00:00:00Z	ru_RU
dc.date.issued	2018	ru_RU
dc.identifier.citation	Ibrahem Yousef., Vladislav Sudakov., Vladimir Morozov., El Kadi Mohammad. STRUCTURAL SETTING AND ZONAL DISTRIBUTION OF UPPER TRIASSIC - LOWER CRETACEOUS RESERVOIRS IN THE SYRIAN EUPHRATES GRABEN//International Multidisciplinary Scientific GeoConference Surveying Geology and Mining Ecology Management, SGEM. - 2018. - Vol.18, Is.1.4. - P.811-818.	ru_RU
dc.identifier.uri	https://repository.kpfu.ru/?p_id=213569	ru_RU
dc.description.abstract	International Multidisciplinary Scientific GeoConference Surveying Geology and Mining Ecology Management, SGEM	ru_RU
dc.description.abstract	The purpose of the article is to assess the regional structure of the upper Triassic - lower Cretaceous sediments (Mulussa F and Rutbah reservoirs), which serve as an important targets for hydrocarbons production and exploration to the center and Middle East of Syria. The upper Triassic - lower Cretaceous sediments are approximately of 800 m thickness consist mainly of floodplain clays interbedded with medium to fine grained fluvial sandstones. In addition, there are dolomites and clay dolomites present in the lower parts of these deposits. The upper Triassic - lower Cretaceous deposits at Euphrates graben area were affected by the tow unconformity erosions; BKL and BKU, which led to significant changes in the thickness of the reservoirs sediments. These changes in thickness are also controlled by the axis of the non-isometric depositional basin, which has a direction from the North-West to the South-East. Another factor controls the changes and distribution of the thickness of upper Triassic - lower Cretaceous zones sediments which are the presence of the two uplifts (Khleissia uplift to the North-East and Rutbah uplift to the South-West). The high thickness of the upper Triassic sediments in the central part of the Euphrates graben suggests that the graben structure was formed prior to the unconformities erosion; BKL and BKU. Lower Cretaceous deposits are preserved almost inside the entire graben with a greater thickness on the flanks of the North-East and South-West of the Euphrates graben axis.	ru_RU
dc.language.iso	ru	ru_RU
dc.subject	Regional	ru_RU
dc.subject	upper Triassic	ru_RU
dc.subject	lower Cretaceous	ru_RU
dc.subject	Euphrates graben	ru_RU
dc.subject	Syria.	ru_RU
dc.title	STRUCTURAL SETTING AND ZONAL DISTRIBUTION OF UPPER TRIASSIC - LOWER CRETACEOUS RESERVOIRS IN THE SYRIAN EUPHRATES GRABEN	ru_RU
dc.type	Статьи в зарубежных журналах и сборниках	ru_RU