KFU. Card publication. Diagenesis of the Mulussa F Sandstone (Upper Triassic), Euphrates Graben, East Syria

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FEDERAL UNIVERSITY

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DIAGENESIS OF THE MULUSSA F SANDSTONE (UPPER TRIASSIC), EUPHRATES GRABEN, EAST SYRIA

Form of presentation

Articles in international journals and collections

Year of publication

2016

Authors, employees of KFU

Morozov Vladimir Petrovich, author

Bibliographic description in the original language

The upper Triassic Sandstone, Mulussa F Formation (MUF) in the Euphrates Graben Fields east of Syria on the Arabian plate continental margin is an oil/gas reservoir. Petrographic analysis combined with X-ray diffraction, and core analysis has been used to assess timing of growth and origin of minerals and cements. Depositional and early diagenetic characteristics of the upper Triassic Sandstone are typical of a fluvial environment. Conspicuous authigenic phases within the sandstones include quartz overgrowths (~5%), kaolinite (up to ~13%), pyrite (0~2%), siderite (up to 24%), ferroan dolomite (up to 37%), anhydrite (0 to 2%), Chlorite (0~2%), Authigenic hair-like Illite (0~2%). The most important of these phases are authigenic quartz and kaolinite, with siderite and dolomite generally only significant on a localized scale. The diagenetic history of MUF sandstones has been greatly influenced by early diagenetic processes which included clay infiltration of sandstones, and the precipitat

Annotation

Journal of current Sciences

Keywords

Diagenesis, Sandstone, Euphrates, Graben, Upper Triassic, Mulussa F, Syria.

The name of the journal

Journal of current Sciences

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

https://repository.kpfu.ru/eng/?p_id=152238&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	The upper Triassic Sandstone, Mulussa F Formation (MUF) in the Euphrates Graben Fields east of Syria on the Arabian plate continental margin is an oil/gas reservoir. Petrographic analysis combined with X-ray diffraction, and core analysis has been used to assess timing of growth and origin of minerals and cements. Depositional and early diagenetic characteristics of the upper Triassic Sandstone are typical of a fluvial environment. Conspicuous authigenic phases within the sandstones include quartz overgrowths (~5%), kaolinite (up to ~13%), pyrite (0~2%), siderite (up to 24%), ferroan dolomite (up to 37%), anhydrite (0 to 2%), Chlorite (0~2%), Authigenic hair-like Illite (0~2%). The most important of these phases are authigenic quartz and kaolinite, with siderite and dolomite generally only significant on a localized scale. The diagenetic history of MUF sandstones has been greatly influenced by early diagenetic processes which included clay infiltration of sandstones, and the precipitat	ru_RU
dc.identifier.uri	https://repository.kpfu.ru/eng/?p_id=152238&p_lang=2	ru_RU
dc.description.abstract	Journal of current Sciences	ru_RU
dc.description.abstract	The upper Triassic Sandstone, Mulussa F Formation (MUF) in the Euphrates Graben Fields east of Syria on the Arabian plate continental margin is an oil/gas reservoir. Petrographic analysis combined with X-ray diffraction, and core analysis has been used to assess timing of growth and origin of minerals and cements. Depositional and early diagenetic characteristics of the upper Triassic Sandstone are typical of a fluvial environment. Conspicuous authigenic phases within the sandstones include quartz overgrowths (~5%), kaolinite (up to ~13%), pyrite (0~2%), siderite (up to 24%), ferroan dolomite (up to 37%), anhydrite (0 to 2%), Chlorite (0~2%), Authigenic hair-like Illite (0~2%). The most important of these phases are authigenic quartz and kaolinite, with siderite and dolomite generally only significant on a localized scale. The diagenetic history of MUF sandstones has been greatly influenced by early diagenetic processes which included clay infiltration of sandstones, and the precipitat	ru_RU
dc.language.iso	ru	ru_RU
dc.subject	Diagenesis	ru_RU
dc.subject	Sandstone	ru_RU
dc.subject	Euphrates	ru_RU
dc.subject	Graben	ru_RU
dc.subject	Upper Triassic	ru_RU
dc.subject	Mulussa F	ru_RU
dc.subject	Syria.	ru_RU
dc.title	Diagenesis of the Mulussa F Sandstone (Upper Triassic), Euphrates Graben, East Syria	ru_RU
dc.type	Articles in international journals and collections	ru_RU