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塔里木盆地顺北地区奥陶系凝析气地球化学特征及成因

崔福田 马安来 云露 曹自成 李贤庆 黄诚 何帅 郭楚媛

崔福田, 马安来, 云露, 曹自成, 李贤庆, 黄诚, 何帅, 郭楚媛. 塔里木盆地顺北地区奥陶系凝析气地球化学特征及成因[J]. 石油实验地质, 2025, 47(5): 1118-1133. doi: 10.11781/sysydz2025051118
引用本文: 崔福田, 马安来, 云露, 曹自成, 李贤庆, 黄诚, 何帅, 郭楚媛. 塔里木盆地顺北地区奥陶系凝析气地球化学特征及成因[J]. 石油实验地质, 2025, 47(5): 1118-1133. doi: 10.11781/sysydz2025051118
CUI Futian, MA Anlai, YUN Lu, CAO Zicheng, LI Xianqing, HUANG Cheng, HE Shuai, GUO Chuyuan. Geochemical characteristics and genesis of Ordovician condensate gas in Shunbei area, Tarim Basin[J]. PETROLEUM GEOLOGY & EXPERIMENT, 2025, 47(5): 1118-1133. doi: 10.11781/sysydz2025051118
Citation: CUI Futian, MA Anlai, YUN Lu, CAO Zicheng, LI Xianqing, HUANG Cheng, HE Shuai, GUO Chuyuan. Geochemical characteristics and genesis of Ordovician condensate gas in Shunbei area, Tarim Basin[J]. PETROLEUM GEOLOGY & EXPERIMENT, 2025, 47(5): 1118-1133. doi: 10.11781/sysydz2025051118

塔里木盆地顺北地区奥陶系凝析气地球化学特征及成因

doi: 10.11781/sysydz2025051118
基金项目: 

国家自然科学基金项目(42272167)、国家自然科学基金企业联合基金项目(U24B6001)、中国石化科技部项目(P23167,P24173)和中央高校基本科研业务费中国矿业大学(北京)博士研究生拔尖创新人才培育基金(BBJ2024044)联合资助。

详细信息
    作者简介:

    崔福田(2000—),女,硕士生,从事油气地质和地球化学研究。E-mail:369556462@qq.com。

    通讯作者:

    马安来(1969—),男,博士,研究员,从事油气地球化学与成藏机理研究。E-mail:maal.syky@sinopec.com。

  • 中图分类号: TE122.112

Geochemical characteristics and genesis of Ordovician condensate gas in Shunbei area, Tarim Basin

  • 摘要: 为了给塔里木盆地顺北地区深层油气勘探提供理论依据,采用气体组分和组分碳、氢同位素分析方法,系统分析了顺北地区奥陶系凝析气化学组成与同位素特征,并与轮古东、玉科及塔中东西部奥陶系凝析气对比,探讨顺北地区凝析气成因及形成过程。顺北地区奥陶系凝析气以烃类气体为主,其中5号断裂带南段、4号断裂带及8号断裂带凝析气干燥系数多低于0.95,呈现湿气特征;而12号断裂带、14号断裂带及顺南地区天然气以干气为主。顺北地区凝析气非烃类气体主要包括少量二氧化碳、氮气及微量硫化氢;烷烃气组分碳、氢同位素序列总体呈正序分布,部分样品出现同位素倒转现象;从5号断裂带南段至顺南地区,天然气成熟度逐渐增加。顺北地区奥陶系凝析气主要为热成因油型气,5号断裂带南段、4号断裂带及8号断裂带天然气为干酪根裂解气与原油裂解气的混合气源,其中原油裂解气以裂解初期形成的湿气为主;12号断裂带、14号断裂带及顺南地区天然气则以高成熟度原油裂解气为主,表现为干气特征。通过天然气地球化学分析,揭示了顺北地区凝析气成因的区域差异性,为塔里木盆地深层油气资源评价和勘探部署提供了依据。

     

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出版历程
  • 收稿日期:  2024-07-23
  • 修回日期:  2025-08-09
  • 刊出日期:  2025-09-28

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