The geochemical data of the gas sourced from the Majiagou Formation indicate low organic content and high thermal maturity, which make the evaluation of the hydrocarbon generative potential difficult. However, the low organic abundance and high thermal maturity of the Majiagou Formation make it difficult to evaluate its hydrocarbon generation potential. The Study of the genesis of pyrite can provide a better understanding of a source rock depositional environment and its evolution. In this paper, we report a significant amount of pyrite linked to the hydrocarbon source in the Majiagou Formation. Light and electron microscopy were used to observe the morphology pyrite while sulfur, carbon, and oxygen isotope were used to investigate the geochemical characteristics of pyrite and the surrounding rock matrix. The results showed that macroscopic stellate pyrite filled cracks and is found in veins or along the laminar surface, as well as agglomerated pyrite; microscopically, pyrite is dominated by autotypic pyrite in the form of cubes, pentagonal dodecahedrons, and columns. The δ 34 S CDT ranged from 4.6‰ to 27.5‰, δ 13 C PDB values ranged from −3.4‰ to −2.3‰, and δ 18 O PDB values ranged from −10.5‰ to −7.3‰. Our findings, combined with the geological background and thermal history of the region, the pyrite in the Majiagou Formation was formed by thermochemical sulfate reduction. Indicating that large-scale hydrocarbon generation events have occurred. The rocks of the Majiagou Formation had the ability to generate hydrocarbons. The research can be utilized as supporting material for the exploration and development of natural gas fields in the Ordos Basin.
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