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    全球天然氢气成因机制、分布规律与地球物理勘探技术进展

    Natural hydrogen: genesis mechanisms, distribution patterns, and progress in geophysical exploration technologies

    • 摘要: 通过系统梳理近年来天然氢气研究进展,构建了完整的成因分类体系,总结了不同成因氢气的主控因素与空间分布规律,并归纳了重磁、地震与测井三类地球物理勘探技术的应用特征。基于全球氢气显示数据与地质要素的叠合分析结果表明: 天然氢气成因可划分为无机成因、有机成因及混合成因三大类,其中无机成因包括水岩反应、断层摩擦生氢、水的电离辐射作用与地球深部脱气四类机制,有机成因包括有机质热解、有机质的电离辐射与微生物作用3类途径,混合成因则为多机制耦合作用;氢气的富集成藏受断裂、岩性组合、盆地类型及输入−输出通量动态平衡的共同控制,无机成因氢气集中于构造活动带及前寒武纪稳定区,有机成因氢气集中于富有机质沉积区,混合成因氢气则常见于构造复杂、多源叠合区域; 在地球物理勘探技术体系中,重磁勘探适于区域尺度氢源岩与基底构造的快速圈定,地震勘探精于储层与断裂系统的空间刻画,测井技术则擅长井孔尺度含氢层段的直接识别与评价。当前天然氢气研究仍面临多来源贡献的精确甄别、全球资源潜力系统预测等挑战,未来需深化氢气成因理论、发展深部探测技术并构建资源预测模型,以支撑规模化天然氢气的资源评价与勘探突破。

       

      Abstract: By systematically reviewing recent advances in natural hydrogen research, this study establishes a comprehensive genetic classification framework, summarizes the controlling factors and spatial distribution patterns of different hydrogen types, and synthesizes the application characteristics of gravity–magnetic, seismic, and well logging techniques. An integrated analysis of global hydrogen occurrence data and geological elements indicates that: hydrogen genesis can be divided into three major types: inorganic, organic, and mixed. Inorganic genesis includes water–rock reactions, fault-related hydrogen generation, water radiolysis, and deep Earth degassing. Organic genesis encompasses thermal maturation, radiolytic decomposition, and microbial activity. Mixed genesis results from the coupling of multiple mechanisms. Hydrogen accumulation is jointly controlled by faults, lithological assemblages, basin types, and the dynamic balance between input and output fluxes. Spatially, inorganic hydrogen is concentrated in tectonically active belts and Precambrian stable zones, organic hydrogen in organic-rich sedimentary areas, and mixed-origin hydrogen in tectonically complex regions with multi-source superimposition. In geophysical exploration, gravity–magnetic surveys excel in rapid regional delineation of hydrogen source rocks and basement structures, seismic exploration in spatial characterization of reservoirs and fault systems, and well logging in direct identification and evaluation of hydrogen-bearing intervals at borehole scale. Current research on natural hydrogen still faces challenges in precisely distinguishing multi-source contributions and systematically assessing global resource potential. Future efforts should focus on advancing hydrogen genesis theories and deep exploration technologies, and developing prediction models to support resource assessment and exploration breakthroughs toward commercial-scale natural hydrogen development.

       

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