四川盆地乐山—龙女寺古隆起气田氦气差异富集特征及地球化学证据OA
Characteristics and geochemical evidence of differential helium enrichment in the gas fields in the Leshan-Longnvsi paleouplift of the Sichuan Basin
四川盆地乐山—龙女寺古隆起威远气田检测到具经济价值的氦气浓度,而安岳气田和资阳气区氦气含量极低,造成这种差异的机制尚不清楚,限制了对古隆起氦气来源及富集规律的深入认识.为此,基于该区天然气地球化学及惰性气体同位素分析结果,结合He和N2的耦合关系,系统探讨了两个气田氦气差异性富集的原因及威远气田氦气富集地质条件.研究结果表明:①两个气田氦气均以壳源为主,威远气田氦气含量(0.18%~0.26%)达工业标准,安岳气田氦气均值较低,且威远气田幔源 3He含量高于安岳气田;②威远、安岳气田震旦系He与N2 相关性良好,威远气田 20Ne与 4He、40Ar与 36Ar含量及比值均显著高于安岳气田,印证两个气田氦气均与地下水密切相关;③资阳地区筇竹寺组烃源岩供氦能力有限,仅凭其放射性衰变难以形成富氦气藏;④威远气田喜马拉雅期构造抬升幅度大,促使基底富氦地下水上升脱溶,且盖层、地层压力及断裂形成的泄压通道实现氦气供给与散失平衡.结论认为,威远气田氦气富集是基底供氦、地下水运移脱溶、喜马拉雅期构造抬升及保存条件协同作用的结果,安岳气田的地质条件则导致气藏难以富集氦气.
Weiyuan gas field,Anyue gas field,and Ziyang gas province are located in the Leshan-Longnvsi paleouplift of the Sichuan Basin.The helium concentration of economic value is detected in Weiyuan gas field,while the helium content is extremely low in Anyue gas field and Ziyang gas province.The mechanisms for this difference have not been figured out,which restricts the deeply understanding on the helium source and enrichment patterns in the paleouplift.Based on the analysis of natural gas geochemistry and noble gas isotopes,combined with the He and N2 coupling relationship,this paper systematically discusses the causes of the differential helium enrichment in Weiyuan and Anyue gas fields,as well as the geological conditions for helium enrichment in Weiyuan gas field.The following results are obtained.First,the helium in both gas fields is mostly crust sourced.The gas content(0.18%-0.26%)in Weiyuan gas field reaches the industrial standard,while that in Anyue gas field is lower.The mantle derived 3He content in Weiyuan gas field is higher than that in Anyue gas field.Second,the Sinian He and N2 are well correlated in Weiyuan and Anyue gas fields,and the 20Ne,4He,40Ar and 36Ar contents and the 20Ne/4He and 40Ar/36Ar ratios in Weiyuan gas field are significantly higher than those in Anyue gas field,which confirms that the helium in these two gas fields are closely related to underground water.Third,the limited helium supply capacity of the Qiongzhusi Formation source rocks in the Ziyang area makes it difficult to form a helium-rich gas reservoir only based on its radioactive decay.Fourth,the large amplitude of structural uplift in Weiyuan gas field during the Himalayan period promoted the ascent and exsolution of the basement helium-rich underground water,and caprock,formation pressure and faulting induced pressure relief channels achieve a balance between helium supply and dissipation.In conclusion,the helium enrichment in Weiyuan gas field is the collaborative product of basement helium supply,underground water migration and exsolution,Himalayan structural uplift and preservation condition,while the geological conditions in Anyue gas field can hardly meet the requirement of He enrichment in the gas reservoirs.
王佳美;秦胜飞;敬江林;戴鑫;汪华;张宝收;豆霜;李晓斌;赵峰华
中国矿业大学(北京)地球科学与测绘工程学院||中国石油勘探开发研究院中国石油勘探开发研究院中国石油西南油气田公司蜀南气矿中国石油西南油气田公司勘探开发研究院中国石油西南油气田公司勘探开发研究院中国石油西南油气田公司勘探开发研究院中国石油西南油气田公司勘探开发研究院中国科学院西北生态环境资源研究院中国矿业大学(北京)地球科学与测绘工程学院
能源科技
四川盆地乐山—龙女寺古隆起氦气差异富集地球化学
Sichuan BasinLeshan-Longnvsi paleoupliftHeliumDifferential enrichmentGeochemistry
《天然气工业》 2026 (3)
69-79,11
深地国家科技重大专项"油气田有关天然气藏中氦气富集与探测"(编号:2025ZD1010500)、国家自然科学基金专项项目"中西部叠合盆地氦气富集机理与资源潜力"(编号:42141022)、国家自然科学基金面上项目"富氦煤层气和页岩气藏氦气富集机理"(编号:42272189)、中国石油股份有限公司项目"中石油探区油气资源潜力、分布规律与勘探方向"(编号:2023YQX201).
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