Analyses
of geochemical characteristics of oil fractions, C-isotope and biological
markers of well cores and crude oil from the Hongqiba area in the northwestern
margin of Junggar Basin reveal that the source rock has low abundance in
organic matter and poor kerogen. Oils from Hongqiba and its adjacent areas show
a certain degree of correlations with the source rocks of the Fengcheng
Formation in the Mahu sag with regard to the distribution of C20, C21,
C23 tricyclic diterpanes, Pr/Ph, and carbon isotope.
Therefore, the authors suggest that oils mainly originated from the
Fengcheng Formation of the Mahu sag.
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