新疆石油地质 ›› 2005, Vol. 26 ›› Issue (5): 513-516.

• 油气勘探 • 上一篇    下一篇

F1断裂在克拉2气田形成与保存中的作用

付广, 祝彦贺, 付晓飞   

  1. 大庆石油学院,黑龙江大庆163318
  • 收稿日期:2005-01-10 出版日期:2005-10-01 发布日期:2020-11-23
  • 作者简介:付广(1962-),男,辽宁新宾人,教授,石油地质,(Tel)0459-6504024(E-mail)fuguang2000@etang.com.

Effect of F1 Fault on Formation and Preservation of Kela-2 Gas Field

FU Guang, ZHU Yan-he, FU Xiao-fei   

  1. Daqing Petroleum Institute, Daqing, Heilongjiang 163318, China
  • Received:2005-01-10 Online:2005-10-01 Published:2020-11-23

摘要: 在FI断裂发育及演化特征分析的基础上,利用 自行设计组装的模报实验装置,对断裂在塔里木盆地克拉2气田形成中的作用进行了模拟,得到Fl断裂在活动时期侏罗系和三叠系源岩生成、排出的天然气向,上运移的通道,但沿其运移散失速度大于其进入克拉2气田内的天然气速度,对克拉2气田形成的贡献不大。通过物理横拟试验确定了膏泥岩塑性变形极限和断裂带封气所需要的膏泥岩舍量下限,利用断层面压力和断裂带中膏泥含量对F1断裂静止后垂向封闭性进行了评价,结果认为,F1断裂在垂向上具有好的封闭性,对克拉2气田中天然气的保存十分有利。

关键词: 塔里木盆地, 克拉2气田, 断裂, 实验, 油气运移, 封闭性

Abstract: The development and evolution of F1 fault is analyzed. The effect of F1 fault on forming Kela-2 gas field in Tarim basin is simulated by using the self-designed model. The pathway for gas migrating upward generated and discharged from Jurassic and Triassic source rocks in active F1 fault. The result shows its lttle contribution to the shape of Kela-2 gas field for the loaing velocity of gas through FI fault zone is bigger than the velocity of gas entering into Kela-2 gas field. The physical model experiment provides the plastic deformation limit of gypsum and mudstone and the minimum contents of gypsum and mudstone to seal gas in F1 fault zone. The fault plane pressure and the contents of gypsum and mudstone are used for evaluation of seal feature in static F1 fault zone, indicating its good vertical seal and favorable preservation for gas accumulation in Kela-2 gas field.

Key words: Tarim basin, Kela-2 gas field, fault, experiment, hydrocarbon migration, seal

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