Tracking the origin of Ordovician natural gas in the Ordos basin using volatile sulfur compounds

Molecular and compound specific isotope analysis of volatile organic sulfur compounds (VOSC), alkanes and CO2 in natural gases from the Ordovician Majiagou Formation of the Daniudi field (Ordos basin, China) was per-formed. The analysis of VOSC demonstrated abundant thiols, sulfides and thiophenes in several samples while others had low concentrations of sulfides only. Molecular analysis of main alkanes and non-hydrocarbons showed the samples vary by the nitrogen and H2S concentrations. Thiols in the gas were at isotopic equilibrium with H2S bearing isotopic signature similar to that of Ordovician anhydrites within the reservoirs, hence the source of H2S was likely thermochemical sulfate reduction (TSR) of these anhydrites. In contrast, gas samples that lacked thiols also lacked H2S. Since all gases came from the same formation and similar thermal regime, the lack of thiols and H2S indicates that the occurrence of TSR in the field was limited, likely by contact between hydrocarbons to the anhydrites. The isotopic signature (834S) of thiophenes in the gas samples suggests the source of the gas is un-likely to be Carboniferous or Permian coals which were previously suggested as the source rocks for the gas. The 813C and 82H of alkanes further supports this suggestion as it demonstrates Carboniferous and Permian gases are unlikely to undergo TSR and generate the gas present in the Ordovician reservoirs. Instead, the 813C and 82H of alkanes hint that the gas source is shale rather than coal.This study demonstrates the applicability of compound specific sulfur isotope analysis of VOSC in identification of H2S sources, performing gas-source rock correlation and acting as a complementary proxy in case where routine analysis of hydrocarbons (813C and 82H) is insufficient for identification of the gas source.