Genesis and crustal constraints of helium in the Kelameili volcanic gas field,Junggar Basin

Li Jiyuan; Qin Shengfei; Tao Gang; Zhao Zizhuo; Yang Haibo; Lu Duo; Gong Deyu; Zhao Fenghua

doi:10.7623/syxb202608014

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Genesis and crustal constraints of helium in the Kelameili volcanic gas field,Junggar Basin

更新时间：2026-09-14

- Genesis and crustal constraints of helium in the Kelameili volcanic gas field,Junggar Basin
- ACTA PETROLEI SINICA Vol. 47, Issue 8, Pages: 1721-1732(2026)
- 作者机构：
  
  1. 中国石油勘探开发研究院,北京,100083
  2. 中国矿业大学(北京)地球科学与测绘工程学院,北京,100083
  3. 中国地质调查局西安地质调查中心,陕西,西安,710119
  4. 中国石油勘探开发研究院西北分院,甘肃,兰州,730020
  5. 大庆油田有限责任公司,黑龙江,大庆,163002
  6. 中国石油新疆油田公司,新疆,克拉玛依,834000
- 作者简介：
- 基金信息：
- DOI：10.7623/syxb202608014
  CLC： TE132.3
- Online First：08 September 2026，
  
  Published：2026
- 稿件说明：
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李济远, 秦胜飞, 陶刚, 赵姿卓, 杨海波, 卢铎, 龚德瑜, 赵峰华. 准噶尔盆地克拉美丽火山岩气田的氦气成因及壳源约束[J]. 石油学报, 2026, 47(8): 1721-1732.

Li Jiyuan, Qin Shengfei, Tao Gang, et al. Genesis and crustal constraints of helium in the Kelameili volcanic gas field,Junggar Basin[J]. ACTA PETROLEI SINICA, 2026, 47(8): 1721-1732.
李济远, 秦胜飞, 陶刚, 赵姿卓, 杨海波, 卢铎, 龚德瑜, 赵峰华. 准噶尔盆地克拉美丽火山岩气田的氦气成因及壳源约束[J]. 石油学报, 2026, 47(8): 1721-1732. DOI： 10.7623/syxb202608014.

Li Jiyuan, Qin Shengfei, Tao Gang, et al. Genesis and crustal constraints of helium in the Kelameili volcanic gas field,Junggar Basin[J]. ACTA PETROLEI SINICA, 2026, 47(8): 1721-1732. DOI： 10.7623/syxb202608014.

摘要

为了认识火山岩天然气藏中氦气的资源类型与分布特征

以准噶尔盆地克拉美丽大型火山岩气田为研究对象

基于气田内代表性天然气样品的He含量、稀有气体和常规天然气的地球化学资料

分析了氦的成因类型及来源

以及火山岩储层中氦的资源潜力。研究结果表明:①克拉美丽气田天然气中的He含量为0.021 4%~0.029 5%

平均为0.026 0%

揭示该气田属贫氦气藏;样品中的

He/

He比值低

样品与大气的

He/

He比值之比为0.024~0.055

揭示天然气中的He组分属于典型的壳源氦

没有明显的幔源氦贡献。②由于克拉美丽气田内火山岩储层的形成时间为石炭纪—二叠纪

远早于其天然气的成藏时间(侏罗纪和白垩纪)

火山活动相关的He元素可能在后期演化中大量散失

对现今气藏中的He组分贡献有限。③克拉美丽气田火山岩储层主要由中性—基性岩组成

这些岩石不仅U、Th等放射性元素含量普遍较低

而且相对于盆地的变质基底

形成年代相对较晚

不利于生成和累积可观的放射性衰变He元素。④生氦量估算和

Ar/

Ar烃源岩年龄约束表明

克拉美丽气田的石炭系煤系烃源岩及相关壳源岩系可能是气藏中壳源氦的重要潜在来源之一。⑤

He与N

存在较好的正相关关系

说明克拉美丽气田的天然气在成藏过程中伴随有地下水的参与

溶解—脱溶过程可能促进了壳源氦从水相进入气相并协同运聚。⑥由于克拉美丽气藏中缺乏与火山活动相关的幔源氦组分

火山岩体自身的原位产氦潜力有限

加之石炭系煤系烃源岩所形成的氦也有限

气藏因氦源不足而贫氦。因此

火山岩气藏不一定能富氦

需根据源、汇、聚的实际条件进行具体分析。

Abstract

To clarify the resource types and distribution patterns of helium in volcanic gas reservoirs

this study investigates the Kelameili large-scale volcanic gas field in Junggar Basin. Based on helium concentrations

noble gas and conventio

nal natural gas geochemical data of representative gas samples collected from the gas field

the genetic mechanisms and sources of helium were determined

and the helium resource potential of volcanic reservoirs was evaluated. The results show as follows. (1) The helium content in the Kelameili gas field ranges from 0.021 4 % to 0.029 5 %

with an average of 0.026 0 %

indicating a helium-poor gas reservoir. The

He/

He ratio in the sample is low

and the ratio to that in the atmosphere ranges from 0.024 to 0.055

indicating a typical crustal origin with no significant contribution from mantle-derived helium. (2) The volcanic reservoirs formed during the Carboniferous-Permian period

which significantly predates the main natural gas accumulation stages in the Jurassic and Cretaceous. Therefore

volcanism-related helium elements may have been extensively lost during subsequent geological evolution

contributing only marginally to the present-day helium in the gas reservoir. (3) The volcanic reservoirs are mainly composed of intermediate-to-mafic rocks

which generally contain low concentrations of radioactive elements such as U and Th. Moreover

these rocks formed later than the metamorphic basement of the basin

making them unfavorable for the long-term generation and accumulation of substantial amounts of radiogenic helium. (4) Helium generation assessments and source rock age constraints inferred from

Ar/

Ar ratios indicate that Carboniferous coal-measure source rocks and associated crustal lithologies may represent important potential sources of crust-derived helium in the gas reservoir. (5) The strong positive correlation between

He and N

suggests the involvement of groundwater during natural gas accumulation. The dissolution and exsolution process may have facilitated the transfer of crustal helium from the aqueous phase into the gas phase

thereby promoting its coupled migration and accumulation with natural gas. (6) The helium deficienc

y of the gas reservoir is primarily attributed to insufficient helium sources

including the absence of significant mantle-derived helium associated with volcanic activity

the limited in-situ helium generation potential of the volcanic rocks

and the negligible helium contribution from Carboniferous coal-measure source rocks. Therefore

volcanic gas reservoirs are not necessarily enriched in helium

and their helium resource potential should be evaluated based on the specific conditions governing helium generation

migration

and accumulation.

关键词

Keywords

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