КФУ. Карточка публикации. Sedimentary and Palaeogeography Evolu-tion of Upper Triassic deposits *Mulussa F Formation* In Euphrates Graben

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SEDIMENTARY AND PALAEOGEOGRAPHY EVOLU-TION OF UPPER TRIASSIC DEPOSITS *MULUSSA F FORMATION* IN EUPHRATES GRABEN &NDASH; SYRIA

Форма представления

Статьи в зарубежных журналах и сборниках

Год публикации

2016

Язык

арабский

Авторы, сотрудники КФУ

Юсеф Ибрахем , автор

Другие авторы

Эль-Кади Мохамад , автор

Библиографическое описание на языке оригинала

Yousef I. M. Sedimentary and Palaeogeography Evolution of Upper Triassic deposits *Mulussa F Formation* In Euphrates Graben – Syria / Ibrahem Yousef, El Kadi Mohammad // Damascus university for basic science. – 2016. – Volume 11, PP, 178-190.

Аннотация

Damascus university for basic science

Ключевые слова

Euphrates Graben, Triassic, Mulussa F, Fluvial, Stratigraphy, Sedimentology, Palaeogeography.

Название журнала

Damascus university for basic science

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https://repository.kpfu.ru/?p_id=216900

Полная запись метаданных

Поле DC	Значение	Язык
dc.contributor.author	Юсеф Ибрахем	ru_RU
dc.contributor.author	Эль-Кади Мохамад	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. M. Sedimentary and Palaeogeography Evolution of Upper Triassic deposits Mulussa F Formation In Euphrates Graben – Syria / Ibrahem Yousef, El Kadi Mohammad // Damascus university for basic science. – 2016. – Volume 11, PP, 178-190.	ru_RU
dc.identifier.uri	https://repository.kpfu.ru/?p_id=216900	ru_RU
dc.description.abstract	Damascus university for basic science	ru_RU
dc.description.abstract	Mulussa F formation constitutes the main part of Upper Triassic deposits in Euphrates Graben. The deeply petrological study of various sediments formation showed that sediments are composed of detrital components as sedimentary members or units forming repeated or harmonic alternations composed of layers whose facies gradients reflect transgression and regression sequences, where the correlation of these sediments led to show their differences and to deduce the distribution patterns with time and place. And thus the study of this formation at area of study enabled to determine the sedimentary and Palaeogeography evolution. The conclusion attained proposed continuous slow periodic sedimentation in a sedimentary basin having variable bathymetry and geometry, controlled by fluctuations in water sea level and meteorological changes besides gradual subsidence. These sediments probably deposited in a sedimentary environment that swing between open marine medium and shallow costal environment with alternating continental and marine conditions. The sediments represent thin barriers near river mouth with curling waterway channels and limited deltaic deposits, locally floating and laterally thinning.	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	Fluvial	ru_RU
dc.subject	Stratigraphy	ru_RU
dc.subject	Sedimentology	ru_RU
dc.subject	Palaeogeography.	ru_RU
dc.title	Sedimentary and Palaeogeography Evolu-tion of Upper Triassic deposits Mulussa F Formation In Euphrates Graben – Syria	ru_RU
dc.type	Статьи в зарубежных журналах и сборниках	ru_RU