Geochemical Characteristics and Origin of Shale Gases From Sichuan Basin, China

• Published in: Frontiers in earth science (Lausanne) Vol. 10
• Main Authors: Ni, Yunyan, Dong, Dazhong, Yao, Limiao, Chen, Jianping, Liang, Xing, Liu, Fei, Li, Jian, Guo, Jinhao, Gao, Jinliang
• Format: Journal Article
• Language: English
• Published: Frontiers Media S.A 22-06-2022
• Subjects: carbon isotope enrichment; carbon isotope reversal; shale gas; Sichuan Basin; Wufeng–Longmaxi shale
• ISSN: 2296-6463; 2296-6463
• DOI: 10.3389/feart.2022.861040

Natural gases from the Taiyang (shallow), Jiaoshiba (middle), and Weirong (deep) shale gas fields in the southern Sichuan Basin were analyzed for molecular and stable carbon isotopic compositions to investigate the geochemical characteristics and gas origins. All the gases belong to shale gas from the Upper Ordovician–Lower Silurian shale and are dominated by methane with gas wetness generally less than 0.83%. The δ
13
C
1
values are −28.5‰, −30.3‰, and −35.2‰ in Taiyang, Jiaoshiba, and Weirong shale gas fields, respectively. The extremely high thermal maturity is the controlling factor for the enrichment of
13
C in methane, with a minor contribution from the heavy carbon isotope of the organic matter in the Ordovician Wufeng Formation. Fischer–Tropsch-type synthesis of hydrocarbon gas from CO
2
and H
2
contributes to the increase of wet gas, which results in the offset from the δ
13
C
1
∼wetness linear trend in the Taiyang and Jiaoshiba gas fields. Methane, ethane, and propane in the Taiyang shale gas field have increasing δ
13
C values with increasing burial depth, which is mainly caused by diffusive migration. All gases are characterized by a complete carbon isotopic reversal trend (δ
13
C
1
> δ
13
C
2
> δ
13
C
3
), and it is mainly caused by the reversible free-radical reactions with the conversion from alkane to alkyl groups, with some contribution from the Fischer–Tropsch-type synthesis. The results of this study will improve our understanding of the geochemical characteristics of shale gases from different burial depths and have important implications for future shale gas exploration in the deep and shallow layers.