Казанский (Приволжский) федеральный университет, КФУ
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DIAGENESIS OF THE MULUSSA F SANDSTONE (UPPER TRIASSIC), EUPHRATES GRABEN, EAST SYRIA
Форма представленияСтатьи в зарубежных журналах и сборниках
Год публикации2016
  • Морозов Владимир Петрович, автор
  • Библиографическое описание на языке оригинала 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
    Аннотация Journal of current Sciences
    Ключевые слова Diagenesis, Sandstone, Euphrates, Graben, Upper Triassic, Mulussa F, Syria.
    Название журнала Journal of current Sciences
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