Geochemical characteristics and origin of natural gas and thermochemical sulphate reduction in Ordovician carbonates in the Ordos Basin, China

Abstract

The Ordos Basin is one of the largest natural gas provinces in China. However, the origin of the gas produced from the Ordovician reservoirs remains puzzling. In order to determine the origin of the Ordovician weathered crust gas in Central Ordos gas field, we analyzed and collated chemical and isotopic data of produced gases along with fluid inclusion homogenization temperatures (HTs), and chemical and isotopic compositions. The weathered crust gas has methane δ 13C 1 similar to the gas derived from Carboniferous–Permian (C–P) coal measures, ethane δ 13C 2 close to the gas in the Ordovician reservoirs below salt (exclusively from Ordovician source rock) in the basin and is the driest gas among all the gases. In contrast to the thermogenic gas model, the gas shows a negative relationship of δ 13C 2 to both the δ 13C 1 and the dryness coefficient. Thus, a hypothesis is proposed that one end-member gas dominated by methane with less negative δ 13C 1 and δD methane but more negative δ 13C 2 has mixed with the other end-member with much less methane and less negative δ 13C 2. The former represents late emplaced gas, likely from post-mature Ordovician sapropelic organic matter with δ 13C of − 27.8‰. The other end-member gas representing less mature gas is derived from highly mature C–P coal measures with δ 13C of − 24.6‰. Post genetic process — thermochemical sulphate reduction (TSR) in the Central Ordos gas field may have resulted in hydrocarbon gas becoming more dominated by methane with isotopically heavier carbon.