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Volume 36 Issue 4
Aug 2025
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Lu Xu, Rui Liu, Yufeng Tang, Kangbin Zhang, Liang Feng, Xiucheng Tan, Fei Liu, Dingchuan Jiang. Geochemical Characteristics of Natural Gas in the Upper Permian Reservoir of the Eastern Sichuan Basin, China: Implication of Multiple Sources Mixing. Journal of Earth Science, 2025, 36(4): 1555-1567. doi: 10.1007/s12583-023-1824-4
Citation: Lu Xu, Rui Liu, Yufeng Tang, Kangbin Zhang, Liang Feng, Xiucheng Tan, Fei Liu, Dingchuan Jiang. Geochemical Characteristics of Natural Gas in the Upper Permian Reservoir of the Eastern Sichuan Basin, China: Implication of Multiple Sources Mixing. Journal of Earth Science, 2025, 36(4): 1555-1567. doi: 10.1007/s12583-023-1824-4

Geochemical Characteristics of Natural Gas in the Upper Permian Reservoir of the Eastern Sichuan Basin, China: Implication of Multiple Sources Mixing

doi: 10.1007/s12583-023-1824-4
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  • Corresponding author: Rui Liu, liurui@outlook.com
  • Received Date: 13 Jun 2022
  • Accepted Date: 05 Feb 2023
  • Available Online: 05 Aug 2025
  • Issue Publish Date: 30 Aug 2025
  • For an improved understanding of gas enrichment mechanism in the eastern Sichuan Basin, South China, twelve natural gas samples were obtained from carbonate reservoirs of the Upper Permian strata to analyze the hydrocarbon and non-hydrocarbon gas compositions, stable carbon and hydrogen isotopes ratios of hydrocarbons, and noble gas isotope ratios. The gas samples in the Upper Permian reservoirs principally consist of alkane gas with a dryness ratio ranging from 127.9 to 1 564.4. The carbon isotope ratio of methane (δ13C1) was almost constant at -34.1 to -31.3‰, but the carbon isotope ratio of ethane (δ13C2) varied from -36.6‰ to -25.8‰. The hydrogen isotope ratio of methane (δ2HC1) also displayed a wide range from -137‰ to -127‰. The large variations in the dryness ratio, δ13C2, and δ2HC1 with almost constant δ13C1 suggest the mixing of sapropelic and humic origins for hydrocarbon gases in these reservoirs. A high concentration of hydrogen sulfide (H2S) originated from the thermochemical sulfate reduction (TSR), which was positively correlated with δ13C1 (or δ13C2) in individual gas fields. TSR altered δ13C1 (or δ13C2) and resulted in the abnormal character of isotopic reversal in the individual samples. The δ13C1 (or δ13C2) in most gas samples, independent of H2S concentration, further displayed reversed carbon isotopes because of the mixture of thermogenic gases with various thermal maturity levels. The measured argon isotope ratio (40Ar/36Ar) varied from 310 to 1 225, which suggests that the oldest 320 Ma source rock age corresponds to Permian shales. The analysis of the gas origin and the identification of primary source rock have made a significant contribution to further understanding the resource potential and distribution of natural gas in the Upper Permian, and have great implications for gas exploration in the eastern Sichuan Basin.

     

  • Conflict of Interest
    The authors declare that they have no conflict of interest.
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