松辽盆地北部氦气富集因素分析

    Analysis of helium enrichment factors in the Northern Songliao Basin

    • 摘要: 松辽盆地北部天然气存在高氦显示,揭示其巨大的氦资源潜力。然而,相较于南部,该区氦气空间分布规律不清、壳源氦主导成因不明、断裂-盖层耦合控藏机制缺乏系统分析,制约了勘探部署。本研究基于53个天然气样品(深度455.4~3 935 m)的高精度氦同位素数据(R/Ra=0.04~1.86),采用R/Ra比值法定量解析气源,综合构造分区、断裂几何参数、盖层物性及岩浆活动开展耦合分析。研究结果表明:①氦气为壳源主导的壳-幔混源成藏,壳源氦平均贡献>75%(R/Ra均值0.92),源自基底花岗岩体放射性衰变;幔源氦占比<25%,受低角度基底断裂(倾角<30°)输导效率限制,通量仅为南部50%。②首次提出幔源氦与总氦含量交汇斜率k>0.3为高效输导阈值,定量揭示低角度断裂控导机制。③青山口组-嫩江组优质盖层是氦气保存关键,浅层氦含量(740 μL/L)较深层(270 μL/L)提升174%。④岩浆-断裂耦合使断裂渗透率提升102~103倍,显著促进幔源氦富集。⑤建立“壳源氦静态累积”与“幔源氦断裂主导”双模式成藏机制,明确南北差异主因是深部输导系统效能不同。本研究系统揭示了松辽盆地北部氦气富集机制,创新性提出低角度断裂控导与动态耦合富集模式,为当地靶区优选及我国类似盆地氦气勘探提供了重要参考。

       

      Abstract: The presence of high-helium shows in natural gas from the Northern Songliao Basin indicates significant helium resource potential. However, compared to the southern part, the spatial distribution patterns of helium remain unclear, the genetic mechanism of crust-derived helium is uncertain, and systematic analysis of fault-caprock coupling control on accumulation is lacking, which constrains exploration deployment. This study is based on high-precision helium isotope data (R/Ra = 0.04-1.86) from 53 natural gas samples (depth: 455.4-3 935 m). The R/Ra ratio method is employed to quantitatively determine gas sources, integrating structural zoning, fault geometric parameters, caprock properties, and magmatic activity for coupling analysis. The results demonstrate that: ①helium accumulation is characterized by crust-dominated, crust-mantle mixed sources, with crustal helium contributing an average of >75% (mean R/Ra = 0.92) from radioactive decay in basement granitic rocks; mantle-derived helium accounts for <25%, limited by the transport efficiency of low-angle basement faults (dip angle <30°), with flux only 50% of the southern basin. ②A slope k>0.3 from the intersection of mantle-derived helium versus total helium content is proposed for the first time as the threshold for efficient transport, quantitatively revealing the low-angle fault control mechanism. ③High-quality mudstone caprocks of the Qingshankou-Nenjiang Formations are crucial for helium preservation, with shallow helium content (740 μL/L) showing a 174% increase compared to deep layers (270 μL/L). ④Magma-fault coupling enhances fracture permeability by 102-103 times, significantly promoting mantle-derived helium enrichment. ⑤A dual accumulation model is established: “static accumulation of crust-derived helium” and “fault-dominated enrichment of mantle-derived helium”, clarifying that the north-south difference stems from deep transport system efficiency variations. This study systematically reveals helium enrichment mechanisms in the Northern Songliao Basin, innovatively proposing low-angle fault control and dynamic coupling enrichment models, providing important reference for local target optimization and helium exploration in similar basins in China.

       

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