Geochemical characteristics and oil–source rock correlation in the Paleogene source rocks of the Qinnan Sag, Bohai Bay basin

The Paleogene Shahejie Formation, including the first (Es<sub>1</sub>) and third (Es<sub>3</sub>) members of the Shahejie Formation, and the third member of Dongying Formation (Ed<sub>3</sub>) are important source rocks in the Qinnan Sag, Bohai Bay Basin. In order to uncover the source of oil and gas in this sag, basic geochemical, molecular geochemical, organic petrological, and <i>n</i>-alkane monomer carbon isotopic characteristics of source rocks and oils were analyzed in detail. In combination with the geological settings, the percentage contribution of these three sets of source rocks was assessed in the Qinnan Sag. Results obtained from the source rocks offered the following insights: (1) total organic carbon (TOC) ranged from 1.0% to 3.0%, and the S<sub>2</sub>-TOC indicated that the qualities of source rocks followed the order of Es<sub>3</sub> > Es<sub>1</sub> > Ed<sub>3</sub>. (2) Organic matter (OM) of the Ed<sub>3</sub> source rock belonged to Type II<sub>2</sub>, while those of Es<sub>1</sub> and Es<sub>3</sub> belonged to Type II<sub>1</sub>. The molecular geochemical parameters (CPI, C<sub>24</sub>TeT/C<sub>26</sub>TT, C<sub>27</sub>-C<sub>29</sub> regular steranes, and 4-MSI) also revealed that the organic matter in the source rocks mainly originated from mixtures of algae and terrestrial higher plants. (3) The % <i>R</i> <sub>o</sub> values of Ed<sub>3</sub>, Es<sub>1</sub>, and Es<sub>3</sub> were 0.61%, 0.80%, and 0.88%, respectively. These results were consistent with the maturity molecular parameters (including <i>T</i>-max, Ts/Tm, C<sub>29</sub>-ααα20<i>S</i>/(20<i>S</i> + 20<i>R</i>) and C<sub>29</sub>-ββ/(ββ + αα)). (4) Pr/Ph, Pr/<i>n</i>C<sub>17</sub>, and Ph/<i>n</i>C<sub>18</sub> values indicated that the three sets of source rocks were deposited in a reduced lacustrine environment with different salinities (analyzed with G/C<sub>30</sub>H), and the salinities of Ed<sub>3</sub> and Es<sub>3</sub> indicated a freshwater brackish water environment, while that of Es<sub>1</sub> suggested a brackish semi-saline water environment. (5) combining the geological settings with the geochemical results of oil-source correlations, it was found that the contribution of Es<sub>1</sub> source rock dominated (>50%) in the sag. Overall, this study provides more accurate data of oil source formation and is significant for oil exploration in the Qinan Sag, Bohai Bay Basin.

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Journal
RSC Advances
Published
2025-01-01
DOI
https://doi.org/10.1039/d5ra01740h
Citations
1
Primary Topic
Hydrocarbon exploration and reservoir analysis
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article
Field-Weighted Citation Impact
0.86

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article

Geochemical characteristics and oil–source rock correlation in the Paleogene source rocks of the Qinnan Sag, Bohai Bay basin

Xukai Shi, Xiaomin Xie
1 citations
RSC Advances
Hydrocarbon exploration and reservoir analysis
0.86
article

Geochemical characteristics and oil–source rock correlation in the Paleogene source rocks of the Qinnan Sag, Bohai Bay basin

Xukai Shi, Xiaomin Xie
article en
1 citations

Abstract

The Paleogene Shahejie Formation, including the first (Es<sub>1</sub>) and third (Es<sub>3</sub>) members of the Shahejie Formation, and the third member of Dongying Formation (Ed<sub>3</sub>) are important source rocks in the Qinnan Sag, Bohai Bay Basin. In order to uncover the source of oil and gas in this sag, basic geochemical, molecular geochemical, organic petrological, and <i>n</i>-alkane monomer carbon isotopic characteristics of source rocks and oils were analyzed in detail. In combination with the geological settings, the percentage contribution of these three sets of source rocks was assessed in the Qinnan Sag. Results obtained from the source rocks offered the following insights: (1) total organic carbon (TOC) ranged from 1.0% to 3.0%, and the S<sub>2</sub>-TOC indicated that the qualities of source rocks followed the order of Es<sub>3</sub> > Es<sub>1</sub> > Ed<sub>3</sub>. (2) Organic matter (OM) of the Ed<sub>3</sub> source rock belonged to Type II<sub>2</sub>, while those of Es<sub>1</sub> and Es<sub>3</sub> belonged to Type II<sub>1</sub>. The molecular geochemical parameters (CPI, C<sub>24</sub>TeT/C<sub>26</sub>TT, C<sub>27</sub>-C<sub>29</sub> regular steranes, and 4-MSI) also revealed that the organic matter in the source rocks mainly originated from mixtures of algae and terrestrial higher plants. (3) The % <i>R</i> <sub>o</sub> values of Ed<sub>3</sub>, Es<sub>1</sub>, and Es<sub>3</sub> were 0.61%, 0.80%, and 0.88%, respectively. These results were consistent with the maturity molecular parameters (including <i>T</i>-max, Ts/Tm, C<sub>29</sub>-ααα20<i>S</i>/(20<i>S</i> + 20<i>R</i>) and C<sub>29</sub>-ββ/(ββ + αα)). (4) Pr/Ph, Pr/<i>n</i>C<sub>17</sub>, and Ph/<i>n</i>C<sub>18</sub> values indicated that the three sets of source rocks were deposited in a reduced lacustrine environment with different salinities (analyzed with G/C<sub>30</sub>H), and the salinities of Ed<sub>3</sub> and Es<sub>3</sub> indicated a freshwater brackish water environment, while that of Es<sub>1</sub> suggested a brackish semi-saline water environment. (5) combining the geological settings with the geochemical results of oil-source correlations, it was found that the contribution of Es<sub>1</sub> source rock dominated (>50%) in the sag. Overall, this study provides more accurate data of oil source formation and is significant for oil exploration in the Qinan Sag, Bohai Bay Basin.

RSC AdvancesVol. 15(27)
Yangtze University (CN)
National Natural Science Foundation of China, China National Offshore Oil Corporation
Openalex Percentile: Top 29%
Hydrocarbon exploration and reservoir analysis
0.86
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