中国鄂尔多斯盆地中东部奥陶系马家沟地层密潭-1 井天然气成因与来源

Qiang Meng , Yu Xiao , Jianglong Shi , Heng Zhao , Yan Liu , Yiqing Wang , Xiaomin Xie , Yaohui Xu
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引用次数: 0

摘要

米坦-1 井在鄂尔多斯盆地中东部奥陶系盐下层天然气勘探方面取得了重大突破,显示奥陶系马家沟组第四系(O1m4)存在高产工业气流。尽管取得了这一成功,但关于在米滩-1 井发现的天然气的来源一直存在争议。测量结果表明,米坦-1 号井的天然气主要由烷烃气体组成(95.18%)。天然气干燥系数(C1/C1-5)为 0.947,H2S 含量为 3.49%,非烃类气体中含有少量 N2 和 CO2。天然气中甲烷、乙烷和丙烷的碳同位素组成分别为-45.5‰、-26.4‰和-24.3‰。根据区域地质背景、潜在源岩特征和天然气地球化学特征,认为米坦-1 井的天然气是奥陶系盐下碳酸盐岩中自生自积的油伴生天然气。然而,某些地球化学异常现象,如甲烷碳同位素值(δ13C1)较轻,乙烷碳同位素值(δ13C2)具有煤炭型天然气特征,引起了人们的质疑。通过对碳氢化合物生成的热模拟实验和岩石中残余气体的分析得出的进一步结论表明,米坦-1 井的特殊地球化学特征与石膏岩的存在有着密切的关系。无处不在的石膏岩具有双重作用:作为有效的盖岩,有利于保留早期生成的天然气,并促进重烃气体(C2+)和 H2S 的生成。相对较低的 H2S 含量(低于 5%)和较高的 C2+ 含量表明,如果存在热化学硫酸盐还原(TSR),其强度不足以对甲烷产生重大影响。δ13C2 被确定为识别 TSR 的潜在敏感参数。
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Genesis and source of natural gas in Well Mitan-1 of Ordovician Majiagou Formation, middle-eastern Ordos Basin, China

The Well Mitan-1 has achieved a major breakthrough in the exploration of Ordovician subsalt natural gas in the mid-eastern Ordos Basin, demonstrating a high-yield industrial gas flow in fourth member of the Majiagou Formation of Ordovician (O1m4). Despite this success, there are ongoing disputes regarding the origin of the natural gas found in Well Mitan-1. Measured results show that the natural gas in Well Mitan-1 is mainly composed of alkane gas (95.18 %). The gas drying coefficient (C1/C1-5) is measured at 0.947, and the H2S content is 3.49 %, with a small amount of N2 and CO2 in the non-hydrocarbon gas. The carbon isotopic compositions of methane, ethane, and propane in the natural gas are −45.5 ‰, −26.4 ‰, and −24.3 ‰, respectively. Based on the regional geological background, the characteristics of potential source rocks and the geochemical characteristics of natural gas, it is considered that the natural gas in Well Mitan-1 is self-generated and self-accumulated oil-associated gas in Ordovician subsalt carbonate rocks. However, certain geochemical anomalies, such as the lighter methane carbon isotope value (δ13C1) and coal-type gas characteristics in ethane carbon isotope (δ13C2), raise questions. Further insights from thermal simulation experiments on hydrocarbon generation and the analysis of residual gas in rocks suggest a close relationship between the special geochemical characteristics of Well Mitan-1 and the presence of gypsum rocks. The ubiquitous gypsum rock serves a dual purpose: acting as an effective caprock, facilitating the retention of early-generated natural gas, and promoting the generation of heavy hydrocarbon gases (C2+) and H2S. The relatively low H2S content (less than 5 %) and higher C2+ content indicate that thermochemical sulfate reduction (TSR), if present, is not strong enough to significantly impact methane. The δ13C2 is identified as a potentially sensitive parameter for identifying TSR.

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