The geochemical composition of oils from Palaeozoic reservoirs in the SE West Siberian Basin

O. V. Serebrennikova, T. Ju Filippova, V. P. Devyatov

    Результат исследований: Материалы для журналаСтатья

    3 Цитирования (Scopus)

    Выдержка

    We present organic geochemical data (vanadyl and Ni-porphyrin contents, pristane/phytane ratios and n-alkane compositions) relating to oils from Palaeozoic reservoirs in the SE West Siberian Basin. Analogous data from organic material in Palaeozoic and overlying Jurassic source rocks is also presented. The Jurassic succession here consists of siliciclastic units deposited during alternating marine transgressions and regressions. Our results indicate that vanadyl and Ni-porphyrins occur predominantly in transgressive units, and that pristane/phytane ratios increase progressively up through the Jurassic section. However, for Jurassic sediments in which vanadyl porphyrins are present, the Pr/Ph ratio is strongly facies dependent and is relatively high in transgressive units and lower in regressive units. By contrast, (C21 + C23 + C25)/3 C20 n-alkane ratios are relatively low in transgressive deposits and higher in regressive deposits. There is a close relationship between this parameter and Pr/Ph ratio. Oils from weathered Palaeozoic reservoirs have variable compositions. In most cases, these compositions appear to be influenced by the depositional characteristics of the overlying Jurassic source intervals. Our data point to a mainly Jurassic origin for the oils in SE Western Siberia. However there is some evidence that a Palaeozoic source may be significant in the south of the studied area.

    Язык оригиналаАнглийский
    Страницы (с-по)465-478
    Число страниц14
    ЖурналJournal of Petroleum Geology
    Том26
    Номер выпуска4
    DOI
    СостояниеОпубликовано - 1 окт 2003

    Отпечаток

    Porphyrins
    Pristane
    Paleozoic
    Jurassic
    porphyrin
    Paraffins
    oil
    Deposits
    Chemical analysis
    basin
    alkane
    Sediments
    Rocks
    transgression
    source rock
    Oils
    sediment

    ASJC Scopus subject areas

    • Earth and Planetary Sciences (miscellaneous)
    • Energy Engineering and Power Technology
    • Fuel Technology

    Цитировать

    The geochemical composition of oils from Palaeozoic reservoirs in the SE West Siberian Basin. / Serebrennikova, O. V.; Filippova, T. Ju; Devyatov, V. P.

    В: Journal of Petroleum Geology, Том 26, № 4, 01.10.2003, стр. 465-478.

    Результат исследований: Материалы для журналаСтатья

    Serebrennikova, O. V. ; Filippova, T. Ju ; Devyatov, V. P. / The geochemical composition of oils from Palaeozoic reservoirs in the SE West Siberian Basin. В: Journal of Petroleum Geology. 2003 ; Том 26, № 4. стр. 465-478.
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    abstract = "We present organic geochemical data (vanadyl and Ni-porphyrin contents, pristane/phytane ratios and n-alkane compositions) relating to oils from Palaeozoic reservoirs in the SE West Siberian Basin. Analogous data from organic material in Palaeozoic and overlying Jurassic source rocks is also presented. The Jurassic succession here consists of siliciclastic units deposited during alternating marine transgressions and regressions. Our results indicate that vanadyl and Ni-porphyrins occur predominantly in transgressive units, and that pristane/phytane ratios increase progressively up through the Jurassic section. However, for Jurassic sediments in which vanadyl porphyrins are present, the Pr/Ph ratio is strongly facies dependent and is relatively high in transgressive units and lower in regressive units. By contrast, (C21 + C23 + C25)/3 C20 n-alkane ratios are relatively low in transgressive deposits and higher in regressive deposits. There is a close relationship between this parameter and Pr/Ph ratio. Oils from weathered Palaeozoic reservoirs have variable compositions. In most cases, these compositions appear to be influenced by the depositional characteristics of the overlying Jurassic source intervals. Our data point to a mainly Jurassic origin for the oils in SE Western Siberia. However there is some evidence that a Palaeozoic source may be significant in the south of the studied area.",
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