Search Results - "Premović, P.I."

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  1. 1

    The vanadium isotopic constitution of petroleum asphaltenes: La Luna Formation (Venezuela) by Premović, P.I., Tonsa, I.R., López, L., Pavlović, M.S., Nešković, O.M., LoMonaco, S., Ðordević, D.M., Veljković, M.V.

    Published in Journal of inorganic biochemistry (30-05-2000)
    “…High-resolution mass spectrometry indicates that the isotopic abundance of 50V of the Late Cretaceous La Luna petroleum asphaltenes of marine origin (highly…”
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    Journal Article
  2. 2

    Vanadium of petroleum asphaltenes and source kerogens (La Luna Formation, Venezuela): isotopic study and origin by PREMOVIC, P. I, DORCEVIC, D. M, PAVLOVIC, M. S

    Published in Fuel (Guildford) (01-10-2002)
    “…High-resolution mass spectrometry indicates that the isotopic abundance of 50vanadium (V) of the Late Cretaceous La Luna petroleum asphaltenes and related…”
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    Journal Article
  3. 3

    Estimation of vanadyl porphyrin concentration in sedimentary kerogens and asphaltenes by Premović, P.I, Allard, T, Nikolić, N.D, Tonsa, I.R, Pavlović, M.S

    Published in Fuel (Guildford) (01-05-2000)
    “…We describe a new, rapid method for determining the concentration of vanadyl porphyrins (VO 2+–P) associated with the kerogen of bituminous sedimentary rocks…”
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    Journal Article
  4. 4

    Electron spin resonance study of the kerogen/asphaltene vanadyl porphyrins: air oxidation by Premović, P.I., Tonsa, I.R., Pajović, M.T., Lopez, L., Monaco, S.L., Đorđević, D.M., Pavlović, M.S.

    Published in Fuel (Guildford) (01-04-2001)
    “…Thermal behavior of vanadyl porphyrins was studied by electron spin resonance during heating of the kerogens isolated from the La Luna (Venezuela), Maganik…”
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    Journal Article
  5. 5

    Incorporation of vanadyl porphyrins into kerogen structures during catagenesis by Premović, P.I, Tonsa, I.R, Đorđević, D.M, Premović, M.P

    Published in Fuel (Guildford) (01-07-2000)
    “…Natural vanadyl (VO2+)–deoxophylloerythroetioporphyrins (DPEP) are shown to be capable of reacting and quantitatively incorporating into the immature kerogen…”
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    Journal Article
  6. 6

    Cretaceous-Paleogene boundary (KPB) Fish Clay at Højerup (Stevns Klint, Denmark): Ni, Co, and Zn of the black marl by P.I. PREMOVIC, B.Ž. TODOROVIĆ, M.N. STANKOVIĆ

    Published in Geologica acta (01-04-2009)
    “…The black marl of the Fish Clay at Højerup is mainly made up of biogenic calcite and cheto-Mg-smectite. We suggest that the formation of the smectite occurred…”
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    Journal Article
  7. 7

    Cretaceous-Paleogene boundary (KPB) Fish Clay at Højerup (Stevns Klint, Denmark): Ni, Co, and Zn of the black marl by Premovic, Pavle I., Todorović, Bratislav Ž., Stanković, Maja N.

    Published in Geologica acta (01-01-2008)
    “…The black marl of the Fish Clay at Højerup is mainly made up of biogenic calcite and cheto-Mg-smectite. We suggest that the formation of the smectite occurred…”
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    Journal Article