Geochemical characteristics and origin of crude oil and natural gas in different areas of Wenchang-A Sag, Pearl River Mouth Basin, South China Sea

Xiaoyan FU, Shijia CHEN, Jungang LU, Mingzhu LEI

PDF(8478 KB)
PDF(8478 KB)
Front. Earth Sci. ›› DOI: 10.1007/s11707-024-1104-3
RESEARCH ARTICLE

Geochemical characteristics and origin of crude oil and natural gas in different areas of Wenchang-A Sag, Pearl River Mouth Basin, South China Sea

Author information +
History +

Abstract

Complex hydrocarbon distributions characterize the Wenchang-A Sag. Systematic study of the geochemical characteristics of crude oil, natural gas and source rocks and their genetic relationship is still needs to be completed. The Rock-Eval, kerogen maceral, vitrinite reflectance, saturated hydrocarbon gas chromatography-mass spectrometry, natural gas components, carbon isotopes, and light hydrocarbon were performed. 1) Crude oil is classified based on four factors: wax content, the presence of C27 diasteranes, the regular steranes αα20RC27-αα20RC28-αα20RC29, and the bicadinanes characteristics. Class I crude oil has high wax and C27 diasteranes. For Class II crude oil, the regular steranes are in ‘L’- shaped distribution, and the content of bicadinanes is shallow. Class III crude oil has soft wax and C27 diasteranes, and regular steranes in the reverse ‘L’-shaped distribution, with a high peak degree of bicadinanes. For Class IV crude oil, regular steranes are in ‘V’-shaped distribution, with high peak bicadinane. 2) Class I crude oil comes from source rocks in area C. Class II crude oil comes from source rocks in areas D and E. Class III crude oil comes from areas A, and B. Class IV crude oil comes from source rocks in area A. 3) The source of natural gas in Group I is hydro propylene, and natural gas in Group II is humic. Natural gas in Group III is mixed. Groups I and II are kerogen cracking gas, and group III is a mixture of crude oil secondary cracking gas and kerogen cracking gas. Natural gas in Groups I and II mainly come from local source rocks, and Group III has mixed source characteristics. In the future, oil exploration can continue in Areas C and D, and more favorable areas for gas exploration are Areas C, D, and E.

Graphical abstract

Keywords

organic geochemistry / origin / geochemical characteristics / crude oil / natural gas

Cite this article

Download citation ▾
Xiaoyan FU, Shijia CHEN, Jungang LU, Mingzhu LEI. Geochemical characteristics and origin of crude oil and natural gas in different areas of Wenchang-A Sag, Pearl River Mouth Basin, South China Sea. Front. Earth Sci., https://doi.org/10.1007/s11707-024-1104-3

References

[1]
Chen L, Fan C W, Liu X Y, Li M, Lei M Z (2021). Hydrocatbon enrichment laws and favourable exploration directions of Wenchang A sag, western Pearl River Mouth Basin.China Offshore Oil and Gas, 33(5): 14–23
CrossRef Google scholar
[2]
Chen Y, Mi T Z, Liu Y T, Li S Q, Zhen Y (2020). Microbial community composition and function in sediments from the Pearl River Mouth Basin.J Ocean Univ China, 19(4): 941–953
CrossRef Google scholar
[3]
Cheng K, Jin W, He Z, Chen J, Yang Z (1987). Composition characteristics of light hydrocarbons in continental oil and condensate and their geological significance.Petrol Explor Dev, 1: 34–43+33
[4]
Cheng P, Xiao X M, Gai H F, Li T F, Zhang Y Z, Huang B J, Wilkins R W T (2015). Characteristics and origin of carbon isotopes of n-alkanes in crude oils from the western Pearl River Mouth Basin, South China Sea.Mar Pet Geol, 67: 217–229
CrossRef Google scholar
[5]
Chung H M, Gormly J R, Squires R M (1988). Origin of gaseous hydrocarbons in subsurface environments: theoretical considerations of carbon isotope distribution.Chem Geol, 71(1−3): 97–104
CrossRef Google scholar
[6]
Dai J (1990). A brief discussion on the problem of the geneses of the carbon isotopic series reversal in organogenic alkane gases.Nat Gas Ind, 10(6): 15–20
[7]
Dehyadegari E (2021). Geochemistry and origins of Sarvak oils in Abadan plain: oil-oil correlation and migration studies.Energy Sources A Recovery Util Environ Effects, 43(6): 716–726
CrossRef Google scholar
[8]
Feng Z, Liu D, Huang S, Gong D, Peng W (2016). Geochemical characteristics and genesis of natural gas in the Yan’an gas field, Ordos Basin, China.Org Geochem, 102: 67–76
CrossRef Google scholar
[9]
Fu N, Li Y C, Sun X, Sun Y M, Xu J Y (2011). Recognition of oil source and source rocks in Zhu III Depression.Geoscience, 25(06): 1121–1130
CrossRef Google scholar
[10]
Gong D, Li J, Ablimit I, He W, Lu S, Liu D, Fang C (2018). Geochemical characteristics of natural gases related to Late Paleozoic coal measures in China.Mar Petrol Geol, 96: 474–500
CrossRef Google scholar
[11]
Hu G, Li J, Li J, Li Z, Luo X, Sun Q, Ma C (2008). Preliminary study on the origin identification of natural gas by the parameters of light hydrocarbon.Sci China Ser D Earth Sci, 51(S1): 131–139
CrossRef Google scholar
[12]
Huang B J, Xiao X M, Zhang M Q (2003). Geochemistry, grouping and origins of crude oils in the Western Pearl River Mouth Basin, offshore South China Sea.Org Geochem, 34(7): 993–1008
CrossRef Google scholar
[13]
HuangD F, LiJ C, ZhouN H, Gu X Z, ZhangD J (1984). The evolution of continental organic matter and the mechanism of hydrocarbon generation. Beijing: Petroleum Industry Press (in Chinese)
[14]
Huang D F, Zhang D J, Li J C (1994). The origin of 4-methyl steranes and pregnanes from Tertiary strata in the Qaidam Basin, China.Org Geochem, 22(2): 343–348
CrossRef Google scholar
[15]
Huang S, Wang Z, Lv Z, Gong D, Yu C, Wu W (2014). Geochemical identification of marine and terrigenous condensates—a case study from the Sichuan Basin, SW China.Org Geochem, 74: 44–58
CrossRef Google scholar
[16]
Huang W B, Cheng J, Shao M L (2022). Discussion on organic matter abundance evaluation criteria of source rocks in deep middle-high thermal evolution stage in south Songliao Basin.Unconventional Oil & Gas, 8(2): 13–23
[17]
HuntJ (1979). Petroleum Geochemistry and Geology. San Francisco: Freeman W. H.
[18]
James A T (1983). Correlation of natural gas by use of carbon isotopic distribution between hydrocarbon components.AAPG Bull, 67(7): 1176–1191
CrossRef Google scholar
[19]
Jiang H, Wang H, Li J L, Chen S P, Lin Z L, Fang X X, Cai J (2009). Research on hydrocarbon pooling and distribution patterns in the Zhu-3 Depression, the Pearl River Mouth Basin.Oil Gas Geol, 30: 275–281+286
[20]
JiangW M, LiY, YangC, Xiong Y Q (2021). Organic geochemistry of source rocks in the Baiyun Sag of the Pearl River Mouth Basin, South China Sea. Marine and Petroleum Geology, 124: 104836
[21]
Leythaeuser D, Schaefer R G, Cornford C, Weiner B (1979). Generation and migration of light hydrocarbons (C2-C7) in sedimentary basins.Org Geochem, 1(4): 191–204
CrossRef Google scholar
[22]
Li X Y, Gong Y (2022). Differences in organic matter between coal and gangue of Shanxi Formation and Taiyuan Formation in Yanchuannan.Unconventional Oil Gas, 9(6): 27–27
CrossRef Google scholar
[23]
Li Y, Chen S J, Wang Y X, Qiu W, Su K M, He Q B, Xiao Z L (2019). The origin and source of the Devonian natural gas in the Northwestern Sichuan Basin, SW China.J Petroleum Sci Eng, 181: 106259
CrossRef Google scholar
[24]
Liu Y, Chen D, Qiu N, Fu J, Jia J (2018). Geochemistry and origin of continental natural gas in the western Sichuan Basin, China.J Nat Gas Sci Eng, 49: 123–131
CrossRef Google scholar
[25]
Lu J G, Luo Z Y, Zou H L, Li Y P, Hu Z Z, Zhou Z Y, Zhu J, Han M M, Zhao L P, Lin , Z H (2021). Geochemical characteristics, origin, and mechanism of differential accumulation of natural gas in the carboniferous kelameili gas field in Junggar Basin, China.J Petroleum Sci Engineering, 203: 108658
CrossRef Google scholar
[26]
Lu K N (2021). Study on classification and evaluation of deep source rocks and their accumulation relations in Dehui Fault Depression.Unconventional Oil Gas, (06): 14–23
CrossRef Google scholar
[27]
MilkovA V (2018). Secondary microbial gas. In: Wilkes H, ed. Hydrocarbons, Oils and Lipids: Diversity, Origin, Chemistry and Fate. Handbook of Hydrocarbon and Lipid Microbiology. Cham: Springer
[28]
Peters K, Cassa M (1994). Applied source rock geochemistry. In: Magoon L, Dow W, eds. AAPG Memoir 60, the Petroleum System - from Source to Trap.AAPG, Tulsa: 93–120
[29]
Prinzhofer A A, Huc A Y (1995). Genetic and post-genetic molecular and isotopic fractionations in natural gases.Chem Geol, 126(3−4): 281–290
CrossRef Google scholar
[30]
QuanY B (2018). Lacustrine source rock development mechanism and its contribution to hydrocarbon accumulation in Zhu III sub-basin, Pearl River Mouth Basin. Dissertation for Doctoral Degree. Wuhan: China University of Geosciences (in Chinese)
[31]
Quan Y B, Liu J Z, Hao F, Bao X H, Xu S, Teng C Y, Wang Z F (2019). Geochemical characteristics and origins of natural gas in the Zhu III subbasin, Pearl River Mouth Basin, China.Mar Pet Geol, 101: 117–131
CrossRef Google scholar
[32]
Quan Y B, Liu J Z, Zhao D J, Hao F, Wang Z F, Tian J Q (2015). The origin and distribution of crude oil in Zhu III sub-basin, Pearl River Mouth Basin, China.Mar Pet Geol, 66(4): 732–747
CrossRef Google scholar
[33]
Su K M, Chen S J, Hou Y T, Zhang H F, Zhang X L, Zhang W X, Liu G L, Hu C, Han M M (2021). Geochemical characteristics, origin of the Chang 8 oil and natural gas in the south western Ordos Basin, China.J Petroleum Sci Eng, 200: 108406
CrossRef Google scholar
[34]
Tang L X, Zhou H, Yin L L (2022). Analysis on organic geochemistry characteristics and hydrocarbon-generating potential of coal-bearing strata in Huaibei Area.Unconventional Oil Gas, 9(6): 51–60,74
CrossRef Google scholar
[35]
Thompson K F M (1983). Classification and thermal history of petroleum based on light hydrocarbons.Geochimica et Cosmochimica Acta, 47(2): 303–316
CrossRef Google scholar
[36]
Tilley B, Mclellan S, Hiebert S, Quartero B, Veilleux B, Muehlenbachs K (2011). Gas isotope reversals in fractured gas reservoirs of the western Canadian Foothills: mature shale gases in disguise.AAPG Bull, 95(8): 1399–1422
CrossRef Google scholar
[37]
TissotB P, WelteD G (1984). Petroleum Formation and Occurrence, second ed. Berlin: Springer-Verlag, 699
[38]
Wang X Z, Cao H X, Cao J (2022). Analysis of natural gas source of Lower Paleozoic in Yan’an Area, Ordos Basin.Unconventional Oil Gas, 9(6): 9–13
CrossRef Google scholar
[39]
Whiticar M (1999). Carbon and hydrogen isotope systematics of bacterial formation and oxidation of methane.Chem Geol, 161(1−3): 291–314
CrossRef Google scholar
[40]
Wood D A, Hazra B J (2017). Characterization of organic-rich shales for petroleum exploration & exploitation: a review-Part 2: geochemistry, thermal maturity, isotopes and biomarkers.J Earth Sci, 28(5): 758–778
CrossRef Google scholar
[41]
Wu C L (1984). Nan Hai (the South China Sea) movement and development of basins in the South China Sea.Mar Sci Bull, 3: 47–53
[42]
Wu L Y, Gu X Z (1986). The application of pyrolysis technique in source rocks research.Acta Petrol Sin, 7(2): 13–19
CrossRef Google scholar
[43]
Xiao X M, Li N H, Gan H J, Tian H, Huang B J, Tang Y C (2009). Tracing of deeply-buried source rock: a case study of the WC9–2 petroleum pool in the Pear River Mouth Basin, South China Sea.Marine Petroleum Geo, 26: 1365–1378
CrossRef Google scholar
[44]
Xiao Z L, Chen S J, Li Y, Su K M, He Q B, Han M M (2020). Local high-salinity source rock and origin of crude oil in the Xianshuiquan Structure in the northwestern Qaidam Basin, China.J Petrol Sci Eng, 198: 108233
CrossRef Google scholar
[45]
XuX D, HuangB J (2000). A Study on the migration and accumulation of oil and gas in Qionghai ulift, Zhusan depression. Petroleum Explor Develop, 27 (4): 41–44+111–120 (in Chinese)
[46]
Zumberge J, Ferworn K, Brown S (2012). Isotopic reversal (‘rollover’) in shale gases produced from the Mississippian Barnett and Fayetteville formations.Mar Petrol Geol, 31(1): 43–52
CrossRef Google scholar

Acknowledgment

Funding for this research came from the Southwest Petroleum University 2021 Graduate Research and Innovation Fund (No. 2021CXYB27), the National Natural Science Foundation of China (Grant Nos. 41872165 and 42072185), and the development mechanism of high-quality source rocks and hydrocarbon accumulation regularity in the Zhusan Depression (No. CCL2020ZJFN0226).

Competing interest:

The authors declare that they have no competing interests.

RIGHTS & PERMISSIONS

2024 Higher Education Press
AI Summary AI Mindmap
PDF(8478 KB)

Accesses

Citations

Detail

Sections
Recommended

/