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塔里木盆地顺托果勒低隆起顺托1井区油气成藏模式

朱秀香 陈绪云 曹自成

朱秀香, 陈绪云, 曹自成. 塔里木盆地顺托果勒低隆起顺托1井区油气成藏模式[J]. 石油实验地质, 2017, 39(1): 41-49. doi: 10.11781/sysydz201701041
引用本文: 朱秀香, 陈绪云, 曹自成. 塔里木盆地顺托果勒低隆起顺托1井区油气成藏模式[J]. 石油实验地质, 2017, 39(1): 41-49. doi: 10.11781/sysydz201701041
Zhu Xiuxiang, Chen Xuyun, Cao Zicheng. Hydrocarbon accumulation mode of Shuntuo 1 well block in the Shuntuoguole lower uplift, Tarim Basin[J]. PETROLEUM GEOLOGY & EXPERIMENT, 2017, 39(1): 41-49. doi: 10.11781/sysydz201701041
Citation: Zhu Xiuxiang, Chen Xuyun, Cao Zicheng. Hydrocarbon accumulation mode of Shuntuo 1 well block in the Shuntuoguole lower uplift, Tarim Basin[J]. PETROLEUM GEOLOGY & EXPERIMENT, 2017, 39(1): 41-49. doi: 10.11781/sysydz201701041

塔里木盆地顺托果勒低隆起顺托1井区油气成藏模式

doi: 10.11781/sysydz201701041
基金项目: 国家科技重大专项(2011ZX050050-004,2011ZXC05002-003)和国家重点基础研究发展计划(973计划)项目(2012CB214806)资助。
详细信息
    作者简介:

    朱秀香(1983-),女,硕士,工程师,从事塔里木盆地油气成藏研究。E-mail:179520361@qq.com。

  • 中图分类号: TE122.3

Hydrocarbon accumulation mode of Shuntuo 1 well block in the Shuntuoguole lower uplift, Tarim Basin

  • 摘要: 塔里木盆地顺托1井区奥陶系碳酸盐岩与志留系碎屑岩层系均获得油气流,为受同一条断裂沟通的2套油气藏,但2套油气藏的地层温度、地层压力系数与油气性质均存在较大差异。通过油气性质、饱和烃色谱、饱和烃色谱—质谱、芳烃色谱—质谱与同位素等地球化学特征对比分析,认为两者为油源相同、多期充注、相互关联的2套油气系统。结合断裂活动期次、断裂活动强度、油气垂向分布特征、油气运移方向及油气充注期次研究,进一步明确志留系油藏主要成藏期为海西晚期,而奥陶系凝析气藏主要成藏期为喜马拉雅期。主要成藏时期断裂的活动强度决定了该区油气富集层系,并初步建立了该区“垂源与侧源供烃、断层垂向输导、断裂活动强度控层、下部圈闭优选聚集”的油气成藏模式。

     

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出版历程
  • 收稿日期:  2016-06-29
  • 修回日期:  2016-12-08
  • 刊出日期:  2017-01-28

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