Форма представления | Статьи в зарубежных журналах и сборниках |
Год публикации | 2016 |
Язык | английский |
|
Морозов Владимир Петрович, автор
|
|
Al-Kadi Mohammad , автор
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Библиографическое описание на языке оригинала |
Sedimentological review of upper Triassic (Mulussa F formation) in Euphrates-graben Syria |
Аннотация |
Journal of Engineering and Applied Sciences |
Ключевые слова |
Euphrates Graben, Triassic, Mulussa F, stratigraphy, sedimentology, chemostratigraphy |
Название журнала |
Journal of Engineering and Applied Sciences
|
URL |
https://www.medwelljournals.com/abstract/?doi=jeasci.2016.3067.3079 |
Пожалуйста, используйте этот идентификатор, чтобы цитировать или ссылаться на эту карточку |
https://repository.kpfu.ru/?p_id=186623 |
Полная запись метаданных |
Поле DC |
Значение |
Язык |
dc.contributor.author |
Морозов Владимир Петрович |
ru_RU |
dc.contributor.author |
Al-Kadi Mohammad |
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 |
Sedimentological review of upper Triassic (Mulussa F formation) in Euphrates-graben Syria |
ru_RU |
dc.identifier.uri |
https://repository.kpfu.ru/?p_id=186623 |
ru_RU |
dc.description.abstract |
Journal of Engineering and Applied Sciences |
ru_RU |
dc.description.abstract |
Journal of Engineering and Applied Sciences |
ru_RU |
dc.description.abstract |
Mulussa F formation is one of the important geological formations constituting the Mulussa group in Syria. The objective of this research is to review of sediments Mulussa F formation. Its deposits contain almost 50% of hydrocarbon potential through Euphrates Graben. Boreholes data permitted confining the formation between two Lithostratigraphic markers and enabled its division into three Lithostratigraphic members MUF3, MUF2, MUF1 (from bottom to top). Each member consists of a set of units, subunits and lithologic intervals. Petrology studying provides a precise petrological description of various formation members and their Digenetic. Results show that the members of the structure are composed of continental detrital sediments made up of clay stones (Kaolinite/Illite) and Shale/Dolomitic clay stone, covered by intervals of quartz sandstones, clay sandstones and silt sandstones. |
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 |
|