KFU. Card publication. Sedimentological Review of Upper Triassic (Mulussa F Formation) In Euphrates Graben

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FEDERAL UNIVERSITY

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

Form of presentation

Articles in international journals and collections

Year of publication

2016

Authors, employees of KFU

Morozov Vladimir Petrovich, author

Other authors

Mohammad El Kadi

Bibliographic description in the original language

Mulussa F Formation (Upper Triassic) is one of the important geological formations constituting the Mulussa Group in Syria. The sediments of this formation spread mainly in the North East part of the country and takes its importance in the Euphrates Graben. Mulussa F deposits form the secondary reservoir and contain almost 50% of the hydrocarbon potential through the area. The petrological investigations and geophysical analyses of well logs enabled to split the formation into three members, from bottom to up; (MUF3, MUF2 and MUF1). Each member consists of a set of units and subunits. Petrological study showed that the sediments of the formation consist of floodplain claystones (kaolinite / illite) interbedded with mostly medium ?grained fluviatile sandstones, lagoonal and shallow-marine dolomitic shales and dolomites are present in the lower and part of the formation. The carbonate sediments are generally absent from the formation sediments unless at the base of the lower member MUF3,

Annotation

Indian journal of science and technology

Keywords

Sedimentology, Upper Triassic, Mulussa F, Euphrates Graben, Syria.

The name of the journal

Indian journal of science and technology

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

https://repository.kpfu.ru/eng/?p_id=152234&p_lang=2

Full metadata record

Field DC	Value	Language
dc.contributor.author	Morozov Vladimir Petrovich	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	Mulussa F Formation (Upper Triassic) is one of the important geological formations constituting the Mulussa Group in Syria. The sediments of this formation spread mainly in the North East part of the country and takes its importance in the Euphrates Graben. Mulussa F deposits form the secondary reservoir and contain almost 50% of the hydrocarbon potential through the area. The petrological investigations and geophysical analyses of well logs enabled to split the formation into three members, from bottom to up; (MUF3, MUF2 and MUF1). Each member consists of a set of units and subunits. Petrological study showed that the sediments of the formation consist of floodplain claystones (kaolinite / illite) interbedded with mostly medium ?grained fluviatile sandstones, lagoonal and shallow-marine dolomitic shales and dolomites are present in the lower and part of the formation. The carbonate sediments are generally absent from the formation sediments unless at the base of the lower member MUF3,	ru_RU
dc.identifier.uri	https://repository.kpfu.ru/eng/?p_id=152234&p_lang=2	ru_RU
dc.description.abstract	Indian journal of science and technology	ru_RU
dc.description.abstract	Mulussa F Formation (Upper Triassic) is one of the important geological formations constituting the Mulussa Group in Syria. The sediments of this formation spread mainly in the North East part of the country and takes its importance in the Euphrates Graben. Mulussa F deposits form the secondary reservoir and contain almost 50% of the hydrocarbon potential through the area. The petrological investigations and geophysical analyses of well logs enabled to split the formation into three members, from bottom to up; (MUF3, MUF2 and MUF1). Each member consists of a set of units and subunits. Petrological study showed that the sediments of the formation consist of floodplain claystones (kaolinite / illite) interbedded with mostly medium ?grained fluviatile sandstones, lagoonal and shallow-marine dolomitic shales and dolomites are present in the lower and part of the formation. The carbonate sediments are generally absent from the formation sediments unless at the base of the lower member MUF3,	ru_RU
dc.language.iso	ru	ru_RU
dc.subject	Sedimentology	ru_RU
dc.subject	Upper Triassic	ru_RU
dc.subject	Mulussa F	ru_RU
dc.subject	Euphrates Graben	ru_RU
dc.subject	Syria.	ru_RU
dc.title	Sedimentological Review of Upper Triassic (Mulussa F Formation) In Euphrates Graben - Syria	ru_RU
dc.type	Articles in international journals and collections	ru_RU