柴达木盆地阿尔金斜坡氦气富集规律及成藏机制OA
Helium enrichment patterns and accumulation mechanisms in the Altyn Slope of the Qaidam Basin
近年来,柴达木盆地阿尔金斜坡多个气田发现高含氦天然气资源,但其氦气富集规律、来源及成藏机制仍存在未明确之处,制约了区域氦气资源的勘探.为此,采集阿尔金斜坡东坪、尖北、昆特依等气田的天然气样品,开展气体组分、碳同位素及稀有气体同位素测试,系统分析氦气地球化学特征、空间分布规律及控制因素,揭示其成藏机制.研究结果表明:①阿尔金斜坡天然气中氦含量呈"边缘隆起高、邻近凹陷低"的特征,且受构造位置、储集层位、基底岩性、气藏埋深及天然气充注过程等多因素控制;②不同天然气田中氦气具有多源供给特征,东坪 3、东坪 1 井区氦气为地壳浅源与深源混合供氦,尖北气田氦气以深部来源为主,东坪 17 井区、牛东和昆特依气田氦气则表现为原位储层或邻近氦源弱源供给;③地层孔隙-裂隙水是氦气运移富集的关键载体,地层水中氦气的积累与基底岩石放射性U、Th元素含量、岩石形成时代及地层水活动性密切相关;④建立阿尔金斜坡3种氦气成藏模式,即多源供氦持续富集模式、远源供氦多期成藏模式及弱源供氦近源成藏模式.结论认为,柴达木盆地阿尔金斜坡氦气富集受构造位置、基底岩性、天然气充注及地层水活动等多因素协同控制,明确的氦气来源、分布规律及成藏模式,可为区域氦气资源潜力评估及针对性勘探开发提供重要理论支撑.
In recent years,helium-rich natural gas resources have been discovered in several gas fields in the Altyn Slope of the Qaidam Basin.However,the helium enrichment patterns,sources and accumulation mechanisms have not been understood completely,which hinders the exploration of helium resources in this area.In this study,natural gas samples collected from Dongping 1,Dongping 3,Jianbei,and Kunteyi gas fields in the Altyn Slope were tested for compositions,carbon isotopes,and noble gas isotopes.Then,the geochemical characteristics,spatial distribution patterns and controlling factors of helium were analyzed systematically,and its accumulation mechanisms were revealed.The following results are obtained.First,the helium content of natural gas in the Altyn Slope exhibits a pattern of"high in marginal uplifts and low in adjacent sags",and it is influenced by multiple factors such as structural position,reservoir horizon,basement lithology,gas reservoir depth,and natural gas charging process.Second,the helium in different gas fields shows multi-source contributions:Dongping 3 and Dongping 1 gas fields feature mixed crustal shallow and deep sources,Jianbei gas field is dominated by deep-source helium,while Dongping 17,Niudong,and Kunteyi gas fields display weak helium supply from in-situ reservoirs or adjacent sources.Third,formation pore-fracture water serves as a key carrier for helium migration and enrichment,and the accumulation of helium in formation water is closely related to the content of radioactive elements U and Th in basement rocks,rock formation age,and formation water activity.Fourth,there are three helium accumulation models in the Altyn Slope:multi-source supply and continuous enrichment,distal supply and multi-stage accumulation,and weak-source supply and proximal accumulation.In conclusion,the helium enrichment in the Altyn Slope of the Qaidam Basin is under the joint control of multiple factors,such as structural position,basement lithology,natural gas charging and formation water activity,and the understanding of helium sources,distribution patterns and accumulation models provides an important theoretical support for the resource potential assessment and targeted exploration and development of helium in this area.
周俊林;白建科;赵明福;李玉宏;杨国军;韩伟;尹菲;徐聃;贺政阳
中国地质调查局西安地质调查中心||中国地质调查局氦气调查研究中心中国地质调查局西安地质调查中心||中国地质调查局氦气调查研究中心青海省地质调查局中国地质调查局西安地质调查中心||中国地质调查局氦气调查研究中心中国石油青海油田公司采气一厂中国地质调查局西安地质调查中心||中国地质调查局氦气调查研究中心西安石油大学地球科学与工程学院中国地质调查局西安地质调查中心||中国地质调查局氦气调查研究中心中国地质调查局西安地质调查中心||中国地质调查局氦气调查研究中心
能源科技
柴达木盆地阿尔金斜坡氦气稀有气体同位素示踪富集规律成藏模式
Qaidam BasinAltyn SlopeHeliumNoble gas isotope tracingEnrichment patternAccumulation model
《天然气工业》 2026 (3)
45-57,13
国家重点研发计划项目"复杂地质介质中氦气运聚及富氦气藏封盖机制研究"(编号:2021YFA0719003),青海省"昆仑英才·高端创新创业人才"特色人才项目"柴达木盆地北缘氦气资源成藏机理及勘探开发"、中国地质调查局项目"氦气资源调查评价与示范"(编号:DD202302002)、陕西省自然科学基金面上项目"热年代学约束下的六盘山盆地海源-固原地区中新生代构造热演化恢复"(编号:2024JC-YBMS-204).
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