Geochemistry of Condensates of Maloyamal’skoe Field (Yamal Peninsula, Western Siberia)

Analysis of distribution of saturated and aromatic hydrocarbon markers identified in five condensates of Maloyamal’skoe field (beds Yu 2–3 , Yu 4 and Yu 6 , Middle Jurassic) leads to the conclusion that their generation is due to lipid components of predominantly terrigenous organic matter (OM) whic...

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Veröffentlicht in:Petroleum chemistry 2019-10, Vol.59 (10), p.1138-1146
Hauptverfasser: Fursenko, E. A., Kim, N. S.
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description Analysis of distribution of saturated and aromatic hydrocarbon markers identified in five condensates of Maloyamal’skoe field (beds Yu 2–3 , Yu 4 and Yu 6 , Middle Jurassic) leads to the conclusion that their generation is due to lipid components of predominantly terrigenous organic matter (OM) which accumulated under weakly reducing conditions. Values of the isomeric ratios of steranes and homohopanes, Ts/Tm, maturity indicators based on the arene composition suggest the formation of condensates under conditions of the main phase of oil generation. Comparison of compositions of condensates and extractable bitumens of dispersed organic matter (DOM) of rocks showed genetic relation of condensates with the organic matter of Middle Jurassic deposits.
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subjects Analysis
Aromatic hydrocarbons
Bituminous materials
Chemistry
Chemistry and Materials Science
Composition
Condensates
Geochemistry
Industrial Chemistry/Chemical Engineering
Lipids
Organic matter
title Geochemistry of Condensates of Maloyamal’skoe Field (Yamal Peninsula, Western Siberia)
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